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Bowes, D. R. (1967) The petrochemistry of some Lewisian granitic rocks. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 342-363 doi:10.1180/minmag.1967.036.279.06

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Reference TypeJournal (article/letter/editorial)
TitleThe petrochemistry of some Lewisian granitic rocks
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsBowes, D. R.Author
Year1967 (September)Volume36
Issue279
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-279-342.pdf+
DOIdoi:10.1180/minmag.1967.036.279.06Search in ResearchGate
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Mindat Ref. ID6087Long-form Identifiermindat:1:5:6087:9
GUID0
Full ReferenceBowes, D. R. (1967) The petrochemistry of some Lewisian granitic rocks. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 342-363 doi:10.1180/minmag.1967.036.279.06
Plain TextBowes, D. R. (1967) The petrochemistry of some Lewisian granitic rocks. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 342-363 doi:10.1180/minmag.1967.036.279.06
In(1966) Mineralogical Magazine Vol. 36 (279) Mineralogical Society
Abstract/NotesSummaryThe chemical compositions of eighty granitic rocks from the Lewisian of the North-West Highlands of Scotland, particularly from the Gairloch district, are set out in relation to geological occurrence and their normative proportions of albite, orthoclase, quartz, and anorthite compared with experimental data relating to the systems NaAlSi3O8-KAlSi3O8-SiO2-H2O and KAlSi3O8-NaAlSi2O8-CaAl2Si2O8-SiO2. The field of composition for these Lewisian rocks moves from Ab-Q-rich for autochthonous granites to Ab = Or = Q (approximately) for parautochthonous granites to Or-rich for intrusive granites. This trend is related to the varying roles of mineral solubility under stress, selective melting, and potassium metasomatism.


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