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Application of the muscovite-paragonite geothermometer to a staurolite-grade schist from Sulitjelma, north Norway

Published online by Cambridge University Press:  05 July 2018

K. J. Henley
K. J. Henley*
Affiliation:
Department of Geology, University College, Gower Street, London, W.C. 1
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Summary

The 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).

Type
Research Article
Information
Mineralogical Magazine , Volume 37 , Issue 290 , June 1970 , pp. 693 - 704
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1970

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Footnotes

1

Present address: The Australian Mineral Development Laboratories, Conyngham St., Frewville, South Australia 5063.

References

Albee, (A. L.), 1965. Phase equilibria in three assemblages of kyanite-zone pelitic schists, Lincoln Mountain Quadrangle, Central Vermont. Journ. Petrology, 6, 246-301.CrossRefGoogle Scholar
Albee, (A. L.) and Chodos, (A. A.), 1965. Microprobe analysis of interlayered muscovite and paragonite, Lincoln Mountain Quadrangle, Vermont. (Abstract. Bull. Geol. Soc. Amer. 78, 2.Google Scholar
Banno, (S.), 1960. Notes on rock-forming minerals (12). Finding of paragonite from the Bessi district, Sikoku, and its paragenesis. Chishitsugaku Zasshi, 66, 123-9.Google Scholar
[Belikovskii, (A. I.)] , 1966. Paragonite from quartz veins on the eastern slopes of the Middle Urals (in Russian). [Mem. All-Union Min. Soc.], 95, 722-6.Google Scholar
Brown, (E. H.), 1967. The greenschist facies in part of Eastern Otago, New Zealand. Contr. Min. Petr. 14, 259-92.CrossRefGoogle Scholar
Burnham, (C. W.) and Radoslovich, (E. W.), 1964. Crystal structures of coexisting muscovite and paragonite. Carnegie Inst. Wash. Yearbook, 63, 232-6.Google Scholar
Butler, (B. C. M.), 1967. Chemical study of minerals from the Moine schists of the Ardnamurchan area, Argyllshire, Scotland. Journ. Petrology, 8, 233 67.CrossRefGoogle Scholar
Chinner, (G. A.), 1960. Pelitic gneisses with varying ferrous/ferric ratios from Glen Clova, Angus, Scotland. Ibid. 1, 178-217.CrossRefGoogle Scholar
Deer, (W. A.), Howie, (R. A.), and Zussman, (S.), 1962. Rock-forming Minerals, 3, Sheet silicates. London (Longmans).Google Scholar
Dietrich, (R. V.), 1958. Chromian muscovite from Baker, Mountain, Virginia. Amer. Min. 43, 162-5.Google Scholar
Ernst, (W. G.), 1963. Significance of phengitic micas from low-grade schists. Ibid. 48, 1357-73.Google Scholar
Ernst, (W. G.), 1964. Petrochemical study of co-existing minerals from low-grade schists, Eastern Shikoku, Japan. Geochimica Acta, 28, 1631-68.CrossRefGoogle Scholar
Eugster, (H. P.) and Yoder, (H. S.) Jr., 1955. The joint muscovite-paragonite. Carnegie lnst. Wash. Yearbook, 54, 124-6.Google Scholar
Guidotti, (C. V.), 1968. On the relative scarcity of paragonite. Amer. Min. 53, 963-74.Google Scholar
Harder, (H.), 1956. Untersuchungen an Paragoniten und an natriumhaltigen Muscoviten. Heidelberger Beitr. Min. Petr. 5, 227-71.Google Scholar
Harte, (B.) and Henley, (K. J.), 1966. Zoned almanditic garnets from regionally metamorphosed rocks. Nature, 210, 689-92.CrossRefGoogle Scholar
Henley, (K. J.), 1968. The Sulitjelma metamorphic complex. Unpublished PhD. thesis, University of London.Google Scholar
Henley, (K. J.), in preparation. The structural and metamorphic history of the Sulitjelma region, N. Norway, with special reference to the nappe hypothesis.Google Scholar
Hietanen, (A.), 1969. Distribution of Fe and Mg between garnet, staurolite and biotite in aluminarich schist in various metamorphic zones north of the Idaho batholith. Amer. Journ. Sci. 267, 422-56.CrossRefGoogle Scholar
Hinterlechner-Ravnik, (A.), 1961. [Paragonite in the dolomitic marble from Cvetkovo Gjubriste, Macedonia. Geol. Razprave Porocila, 7, 233-6.] Abstract No. 7730b 1. Chem. Abstr. 58, 1963.Google Scholar
Hunziker, (J. C.), 1966. Zur Geologie und Geochemie des Gebietes zwischen Valle Antigorio (Provincia di Novara) und Valle di Campo (Kt. Tessin). Schweiz. Min. Petr. Mitt. 46, 473-552.Google Scholar
Hutton, (C. O.), 1940. Optical properties and chemical composition of two micas from Westland, South Island, New Zealand. N.Z. Journ. Sci. Technol., sec. B, 21, 330-1.Google Scholar
Iiyama, (J. T.), 1964. Étude des réactions d'éhange d'ions Na-K dans la série muscovite-paragonite. Bull. Soc. franç. Min. Crist. 87, 532-41.Google Scholar
Lambert, (R. S. T. J.), 1959. The mineralogy and metamorphism of the Moine schists of the Morar and Knoydart districts of Inverness-shire. Trans. Roy. Soc. Edin. 63, 553-88.CrossRefGoogle Scholar
Mason, (R.), 1966. The Sulitjelma gabbro complex. Unpublished Ph.D. thesis, University of Cambridge.Google Scholar
Mason, (R.), 1967. The field relations of the Sulitjelma gabbro. Norsk. Geol. Tidsskr. 47, 237-48.Google Scholar
McNamara, (M.), 1965. The lower greenschist facies in the Scottish Highlands. Geol. För. Förh. 87, 347-89.CrossRefGoogle Scholar
Miyashiro, (A.), 1962. Notes on rock-forming minerals. (22) Common occurrence of muscovite rich in iron and magnesium in glaucophanitic metamorphic terrains. Journ. Geol. Soc. Japan, 68, 234-5.CrossRefGoogle Scholar
Muller, (L. D.) and Burton, (C. J.), 1965. The heavy liquid density gradient and its application to ore dressing mineralogy. Proc. VIIIth Commonwealth Min. Metall. Congr., Austr. and N.Z. 6, 1151-63.Google Scholar
Neumann, (H.), 1959. Contributions to the mineralogy of Norway. No. I. An introduction. Norsk. Geol. Tidsskr. 39, 231-6.Google Scholar
Nicholson, (R.), 1967. On the relations between volcanic and other rocks in the fossiliferous east Lomivann area of Norwegian Sulitjelma. Norges Geol. Unders. 242, 143-56.Google Scholar
Nicol, (A. W.) and RoY, (R.), 1965. Some observations on the system muscovite-paragonite. Canad. Journ. Earth Sci. 2, 401-5.CrossRefGoogle Scholar
Popov, (A. A.) , 1967. Synthesis of muscovite and paragonite at temperatures of 350 to 500°C Geochemistry International (English translation), 4, 964-70.Google Scholar
Popov, (A. A.), 1968. Composition of muscovites and paragonites synthesized at temperatures of 350° to 500°. Ibid. 5, 94-105.Google Scholar
Richardson, (S. W.), 1968. Staurolite stability in a part of the system Fe–A1–Si–O–H. Journ. Petrology, 9, 467-88.CrossRefGoogle Scholar
Rosenfelo, (J. L.), Thompson, (J. B.), and Zen, (E-AN), 1958. Data on co-existent muscovite and paragonite (Abstract). Bull. Geol. Soc. Amer. 69, 1637.Google Scholar
Saxena, (S. K.), 1966. Distribution of elements between co-existing muscovite and biotite and the crystal chemical role of titanium in micas. Neues Jahrb. Min., Abh. 105, I-17.Google Scholar
Schaller, (W. T.) and Stevens, (R. E.), 1941. The validity of paragonite as a mineral species. Amer. Min. 26, 541-5.Google Scholar
Sollas, (W. J.), 1891. A method of determining specific gravity. Nature, 43, 404; see also idem, ibid. 49, 211 (1893) an. Quart. Journ. Geol. Soc. 58, 163 (1902).CrossRefGoogle Scholar
Vogt, (TH.), 1927. Sulitelmafeltets geologi og petrografi. Norges Geol. Unders. 121.Google Scholar
Wilson, (M. R.), 1968. An investigation of supposed nappe structure on the north side of Langvann, Sulitjelma, North Norway. Unpublished Ph.D. thesis. University of Manchester.Google Scholar
Yakshin, (V. I.) , 1964. [Paragonite from rutile amphibolites of the Central Urals. Tr. Sverdlovskogo Gorn. Inst. 45, 36-9.] Abstract No. a757g in Chem. Abstr. 63, 1965.Google Scholar
Zen, (E-AN) and Alree, (A. L.), 1964. Co-existent muscovite and paragonite in pelitic schists. Amer. Min. 49, 904-25.Google Scholar
Zen, (E-AN), Ross, (M.), and Bearth, (P.), 1964. Paragonite from the Täsch valley near Zermatt, Switzerland. Ibid. 183-90.Google Scholar