| Reference Type | Journal (article/letter/editorial) |
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| Title | Application of the muscovite-paragonite geothermometer to a staurolite-grade schist from Sulitjelma, north Norway |
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| Journal | Mineralogical Magazine |
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| Authors | Henley, K. J. | Author |
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| Year | 1970 (June) | Volume | 37 |
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| Issue | 290 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-290-693.pdf+ |
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| DOI | doi:10.1180/minmag.1970.037.290.07Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6367 | Long-form Identifier | mindat:1:5:6367:2 |
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| GUID | 0 |
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| Full Reference | Henley, K. J. (1970) Application of the muscovite-paragonite geothermometer to a staurolite-grade schist from Sulitjelma, north Norway. Mineralogical Magazine, 37 (290) 693-704 doi:10.1180/minmag.1970.037.290.07 |
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| Plain Text | Henley, K. J. (1970) Application of the muscovite-paragonite geothermometer to a staurolite-grade schist from Sulitjelma, north Norway. Mineralogical Magazine, 37 (290) 693-704 doi:10.1180/minmag.1970.037.290.07 |
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| In | (1970, June) Mineralogical Magazine Vol. 37 (290) Mineralogical Society |
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| Abstract/Notes | SummaryThe occurrence of coexisting paragonite (containing 0·70 % CaO) and muscovite (containing 0·16 % CaO) in a staurolite-grade paragonite-muscovite-hornblende-garnet-biotite schist from Sulitjelma enables an estimate to be made of the temperature of recrystallization, using an extension, based on crystal chemistry considerations and available analyses of muscovites and paragonites from metamorphic rocks, of the experimentally determined solvus in the K-Na white mica system into the Ca-K-Na system. This temperature of recrystallization is approximately 550–70 °C and is consistent with the experimental data on the coexistence of staurolite and quartz in the system Fe-A1-Si-O-H (Richardson, 1968). |
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