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Thomas, L. J., Harmon, R. S., Oliver, G. J. H. (1985) Stable isotope compositions of alteration fluids in low-grade Lower Palaeozoic rocks, English Lake District. Mineralogical Magazine, 49 (352) 425-434 doi:10.1180/minmag.1985.049.352.13

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Reference TypeJournal (article/letter/editorial)
TitleStable isotope compositions of alteration fluids in low-grade Lower Palaeozoic rocks, English Lake District
JournalMineralogical MagazineISSN0026-461X
AuthorsThomas, L. J.Author
Harmon, R. S.Author
Oliver, G. J. H.Author
Year1985 (June)Volume49
Issue352
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_49/49-352-425.pdf+
DOIdoi:10.1180/minmag.1985.049.352.13Search in ResearchGate
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Mindat Ref. ID3748Long-form Identifiermindat:1:5:3748:2
GUID0
Full ReferenceThomas, L. J., Harmon, R. S., Oliver, G. J. H. (1985) Stable isotope compositions of alteration fluids in low-grade Lower Palaeozoic rocks, English Lake District. Mineralogical Magazine, 49 (352) 425-434 doi:10.1180/minmag.1985.049.352.13
Plain TextThomas, L. J., Harmon, R. S., Oliver, G. J. H. (1985) Stable isotope compositions of alteration fluids in low-grade Lower Palaeozoic rocks, English Lake District. Mineralogical Magazine, 49 (352) 425-434 doi:10.1180/minmag.1985.049.352.13
In(1985, June) Mineralogical Magazine Vol. 49 (352) Mineralogical Society
Abstract/NotesAbstractA combination of hydrogen and oxygen isotope analyses and fluid inclusion studies has defined the composition of fluids involved in the metamorphism of Lower Palaeozoic rocks in the English Lake District. Three fluid fields have been defined from secondary phases: 1, syn-burial metamorphic D-enriched fluids from epidote and chlorite at a temperature between 250 and 350°C; D-depleted fluid measured from groundmass and quartz inclusions; 3, a mixed magmatic-meteoric fluid with an intermediate H-isotopic composition estimated from W/R granite data and calculated from illite.


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