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Batchelor, R. A., Armstrong, D. C., McDonald, M. (1992) Composition of fluids in quartz: discrimination of magma pulses in a Caledonian granitoid. Mineralogical Magazine, 56 (384) 335-342 doi:10.1180/minmag.1992.056.384.05

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Reference TypeJournal (article/letter/editorial)
TitleComposition of fluids in quartz: discrimination of magma pulses in a Caledonian granitoid
JournalMineralogical MagazineISSN0026-461X
AuthorsBatchelor, R. A.Author
Armstrong, D. C.Author
McDonald, M.Author
Year1992 (September)Volume56
Issue384
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-384-335.pdf+
DOIdoi:10.1180/minmag.1992.056.384.05Search in ResearchGate
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Mindat Ref. ID1837Long-form Identifiermindat:1:5:1837:5
GUID0
Full ReferenceBatchelor, R. A., Armstrong, D. C., McDonald, M. (1992) Composition of fluids in quartz: discrimination of magma pulses in a Caledonian granitoid. Mineralogical Magazine, 56 (384) 335-342 doi:10.1180/minmag.1992.056.384.05
Plain TextBatchelor, R. A., Armstrong, D. C., McDonald, M. (1992) Composition of fluids in quartz: discrimination of magma pulses in a Caledonian granitoid. Mineralogical Magazine, 56 (384) 335-342 doi:10.1180/minmag.1992.056.384.05
In(1992, September) Mineralogical Magazine Vol. 56 (384) Mineralogical Society
Abstract/NotesAbstractFluids trapped inside fluid inclusions in quartz from the multiphase Starav monzogranite in Etive, Argyll, were extracted under vacuum and quantitative data for H2O and CO2 were obtained manometrically. Na and K were determined on an aqueous leach from the decrepitated grains. A bivariate diagram of H2O/CO2 versus Na/K discriminates between magma pulses and mirrors the whole-rock trace-element chemistry. This work shows that compositional variations of fluids in quartz from a weakly mineralised granitoid intrusion are sensitive indicators of its magmatic history and identify subtle changes in its mineralogical composition.


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