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On micas from magmatic and metamorphic rocks

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Abstract

Micas from magmatic and metamorphic rocks differ from one another in chemical composition and in trace element content. The chemical composition of micas is discussed in relation to their occurrence, paragenesis and sequence of crystallization. On the basis of previous studies of the relationship between the physical properties and the chemical composition of 34 chemically analysed micas, reliable physical methods have been established which permit identification of different mica varieties in the same rock. Structural formulae and trace element content of micas from basic and granitic rocks, as well as from skarns, schists, ortho- and paragneisses are discussed. The relationship between the components of the tetrahedral and octahedral layers and of the interlayer are illustrated as ratios.

Poorly differentiated, hybrid and metasomatic rocks often contain more than one variety of mica. Some prophyritic basalts and lamprophyres contain an early phlogopite which is paragenetically related to pyroxene phenocrysts and late biotite which occurs in the groundmass and in the fractures as a result of the crystallization of residual magma. The biotitemuscovite assemblage was observed in granodiorites, quartz-monzonites, schists and gneisses. In the albite-K-feldspar granites, muscovite predominates and the biotite is usually altered.

The chemical composition of micas from metamorphic rocks depends on the grade of metamorphism and on the nature of associated minerals. The biotite from paragneisses contains considerable quantities of octahedral alumina. Pre-metamorphic micas show variable deficiencies of the (OH, F) group. The micas are useful minerals in determining the degree of differentiation and subsequent alteration of igneous rocks.

The present study was carried out on the basis of 34 recent complete chemical analyses andca 100 X-ray fluorescence analyses.

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References

  • Amirkhanoff, K. I., S. B. Brandt andE. N. Bartinsky: Radiogenic argon in minerals and its migration. Ann. N.Y. Acad. Sci.91 (Art. 2), 235–275 (1961).

    Article  Google Scholar 

  • Brun, A.: Note sur l’hydration des micas. Bull. S.I. Soc. franç. minéral36, 44 (1913).

    Google Scholar 

  • Correns, C. W.: Experiments on the decomposition of silicates and discussion of chemical weathering. Clays and Clay Minerals10, 443–459 (1963).

    Article  Google Scholar 

  • Ellisworth, H. V.: Rare element minerals of Canada. Geol. Survey, Canada, Econ. Geol. Ser.11 (1932).

  • Eskola, P.; in:T. F. W. Barth, C. W. Correns andPentti Eskola, Die Entstehung der Gesteine. Berlin: Springer 1939.

    Google Scholar 

  • —— The mica of the moro. Bull. comm. géol. Finlande144, 113–116 (1949).

    Google Scholar 

  • Eugster, H. P., andD. R. Wones: Stability relations of the ferruginous biotite, annite. J. Petrology3, No 1, 82–125 (1962).

    Google Scholar 

  • Foster, M. D.: Interpretation of the composition of trioctahedral micas. U.S. Geol. Survey Prof. Paper354-B, 11–49 (1960).

    Google Scholar 

  • Fröhlich, F.: Beitrag zur Geochemie des Chroms. Geochim. et Cosmochim. Acta20, 215–240 (1960).

    Article  Google Scholar 

  • Goldschmidt, V. M.: Geochemistry. Ed. Alex Muir. Oxford: Clarendon Press 1954.

    Google Scholar 

  • Heinrich, E. W.: Studies in the mica group. Am. J. Sci.244, 836–848 (1946).

    Article  Google Scholar 

  • --A. A. Levinson, D. W. Levandowski andC. H. Hewitt: Studies in the natural history of micas. Project M-978 (1951–1953). University of Michigan. Engineering Research Institute. Ann Arbor 1953.

  • Hewitt, D. F.: Geology of Cardiff and Faraday townships. Ann. Rept Ontario Dept Mines.66, pt. 3 (1957).

  • Jäger, E., E. Kempter, E. Niggli u.H. M. Wüthrich: Biotit-Varietäten und Stilpnomelan in Alpinmetamorph überprägten Mittagfluh-Granit (Aarmassiv). Schweiz. mineral. petrogr. Mitt.4, H. 1, 117–126 (1961).

    Google Scholar 

  • Kretz, R.: Chemical study of garnet, biotite, and hornblende from gneisses of southwestern Quebec, with emphasis on distribution of elements in coexisting minerals. J. Geol.67, No 4, 371–402 (1959).

    Article  Google Scholar 

  • Lowdon, J. A.: Age determinations by the Geological Survey of Canada; Report 1 — Isotopic ages. Geol. Survey, Canada, Paper 60-17 (1960).

    Google Scholar 

  • —— Age determinations by the Geological Survey of Canada; Report 2 — Isotopic ages. Geol. Survey, Canada, Paper 61-17 (1961).

    Google Scholar 

  • ——C. H. Stockwell, H. W. Tipper andR. K. Wanless: Age determinations and geological studies (incl. Report 3 — Isotopic ages). Geol. Survey, Canada, Paper 62-17 (1963).

    Google Scholar 

  • Métais, D., J. Ravier etPhan-Kien-Duong- Nature et composition chimique des micas des deux lamprophyres. Bull. Soc. fran. minéral. et crist.85, No 4, 321–328 (1962).

    Google Scholar 

  • Nockolds, S. R.: The relation between chemical composition and paragenesis in the biotite micas of igneous rocks. Am. J. Sci.245, 401–420 (1947).

    Article  Google Scholar 

  • ——, andR. L. Mitchell: The geochemistry of some Caledonian plutonic rocks. A study in the relationship between the major and trace elements of igneous rocks and their minerals. Proc. Roy. Soc. Edinburgh, Trans.61, Pt. II, No 17, 533–573 (1946).

    Google Scholar 

  • Platen, H. V., u.H. G. F. Winkler: Kristallisation eines Obsidians bei Anwesenheit von H2O, NH3 HCl, und HF unter 2000 Atm. Druck. Fortschr. Mineral.39, 355 (1961).

    Google Scholar 

  • Reesor, J. E.: Dewar creek map area, British Columbia. Geol. Survey, Canada, Memoir292 (1958).

    Google Scholar 

  • Rimšaite, J.: Studies of rock-forming micas (abstract). Am. Mineralogist47, 201 (1962).

    Google Scholar 

  • —— Studies of rock-forming micas. Geol. Survey, Canada, Bull. (1963) (in press).

    Google Scholar 

  • Rinne, F.: Röntgenographische Diagnostic beim Brennen von Kalkstein, Dolomit, Kaolniti und Glimmer. Z. Kristall.61, 113–124 (1924).

    Google Scholar 

  • Satterly, J.: Radioactive mineral occurrences in the Bancroft area. Ann. Rept Ontario Dept Mines65, pt. 6 (1956).

  • Stockwell, C. H.: A tectonic map of the Canadian Shield. Royal Soc. Canada, Spec. Publ.4, 5–15 (1962).

    Google Scholar 

  • Tsvetkov, A. I., andE. P. Valyashikhina: Data on thermal studies of minerals. III. Micas. Trans. Inst. Geol. Mining, Mineral. Geoch., edit. 4. Moscow: Acad. Sci. U.S.S.R. 1956.

    Google Scholar 

  • Yoder, H. S., andH. P. Eugster: Phlogopite synthesis and stability ranges. Geochim. Acta6, 157–185 (1954).

    Article  Google Scholar 

  • —— —— Synthetic and natural muscovites. Geochim. et Cosmochim. Acta8, 227–271 (1955).

    Google Scholar 

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Dedicated to Professor Dr.Carl W. Correns on the occasion of his 70th birthday.

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Rimšaite, J. On micas from magmatic and metamorphic rocks. Beitr Mineral u Petrogr 10, 152–183 (1964). https://doi.org/10.1007/BF02652613

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