| Reference Type | Journal (article/letter/editorial) |
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| Title | Subsolidus crystallization behaviour in the system KAlSi3O8–NaAlSi3O8–H2O |
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| Journal | Mineralogical Magazine |
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| Authors | Parsons, Ian | Author |
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| Year | 1969 (June) | Volume | 37 |
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| Issue | 286 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-286-173.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.286.03Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6252 | Long-form Identifier | mindat:1:5:6252:1 |
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| GUID | 0 |
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| Full Reference | Parsons, Ian (1969) Subsolidus crystallization behaviour in the system KAlSi3O8–NaAlSi3O8–H2O. Mineralogical Magazine, 37 (286) 173-180 doi:10.1180/minmag.1969.037.286.03 |
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| Plain Text | Parsons, Ian (1969) Subsolidus crystallization behaviour in the system KAlSi3O8–NaAlSi3O8–H2O. Mineralogical Magazine, 37 (286) 173-180 doi:10.1180/minmag.1969.037.286.03 |
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| In | (1969, June) Mineralogical Magazine Vol. 37 (286) Mineralogical Society |
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| Abstract/Notes | SummaryWhen gels and glasses of alkali feldspar composition are crystallized hydrothermally below their solidus the crystals present when crystallization is incomplete do not have the same Na:K ratio as the starting material but bear a relation to the starting material analogous to that between crystals and liquids coexisting at the liquidus. This effect has been investigated in the temperature range 700–850 °C at water-vapour pressures between 5000 lb/in.2 and 30000 lb/in.2 Fractionation and normal zoning of crystals may, in principle, occur within fixed bulk compositions held under isothermal, isobaric conditions. |
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