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Carmichael, I. S. E. (1962) Pantelleritic liquids and their phenocrysts. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (257) 86-113 doi:10.1180/minmag.1962.033.257.03

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Reference TypeJournal (article/letter/editorial)
TitlePantelleritic liquids and their phenocrysts
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsCarmichael, I. S. E.Author
Year1962 (June)Volume33
Issue257
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_33/33-257-86.pdf+
DOIdoi:10.1180/minmag.1962.033.257.03Search in ResearchGate
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Mindat Ref. ID5674Long-form Identifiermindat:1:5:5674:2
GUID0
Full ReferenceCarmichael, I. S. E. (1962) Pantelleritic liquids and their phenocrysts. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (257) 86-113 doi:10.1180/minmag.1962.033.257.03
Plain TextCarmichael, I. S. E. (1962) Pantelleritic liquids and their phenocrysts. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (257) 86-113 doi:10.1180/minmag.1962.033.257.03
In(1962) Mineralogical Magazine Vol. 33 (257) Mineralogical Society
Abstract/NotesSummaryThe phenocrysts of four porphyritic obsidians from Pantelleria have been analysed chemically, together with the residual glasses (liquids). Three new analyses of anorthoclase (one partial analysis), two of sodic ferrohedenbergite, one of fayalitic olivine, and two of cossyrite are presented together with their optical properties, and the relationship of these phenocrysts to their liquids is considered.The experimental studies in the system NaAlSi3O8-KAlSi3O8-SiO2-H2O show that for synthetic liquids of similar composition to the normative salic constituents of the pantelleritic liquids, a potassic alkali feldspar crystallizes, whereas in the pantelleritic liquids phenocrysts of anorthoclase (Ab67–Ab61) occur. It is suggested that sodium metasilicate, which appears in the norms of all the pantelleritic liquids, may be responsible for the divergence in trend between the synthetic feldspar-liquid tie-lines and the pantelleritic feldspar-liquid tie-lines.


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