| Reference Type | Journal (article/letter/editorial) |
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| Title | Anorthoclase megacrysts: physical conditions of formation |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Bahat, Dov | Author |
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| Year | 1979 (June) | Volume | 43 |
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| Issue | 326 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_43/43-326-287.pdf+ |
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| DOI | doi:10.1180/minmag.1979.043.326.11Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3022 | Long-form Identifier | mindat:1:5:3022:3 |
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| GUID | 0 |
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| Full Reference | Bahat, Dov (1979) Anorthoclase megacrysts: physical conditions of formation. Mineralogical Magazine, 43 (326) 287-291 doi:10.1180/minmag.1979.043.326.11 |
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| Plain Text | Bahat, Dov (1979) Anorthoclase megacrysts: physical conditions of formation. Mineralogical Magazine, 43 (326) 287-291 doi:10.1180/minmag.1979.043.326.11 |
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| In | (1979, June) Mineralogical Magazine Vol. 43 (326) Mineralogical Society |
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| Abstract/Notes | SummaryPrevious interpretations relating to precipitation of anorthoclase megacrysts from alkaline basaltic magmas under high-pressure conditions are contradicted. It is proposed that these feldspars were crystallized above the solvus from hydrous melts at shallow depths, under low-pressure equilibrium conditions. These melts had been considerably enriched with volatiles of sodium, strontium, and barium, and to some extent also of rubidium. |
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