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Growth twinning in phacolite

Published online by Cambridge University Press:  05 July 2018

Mizuhiko Akizuki
Affiliation:
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University, Sendai 980, Japan
Hiroshi Konno
Affiliation:
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University, Sendai 980, Japan

Abstract

Phacolite from Mitaki, Sendai City, Japan, has a core of penetration-twinned chabazite. The crystal has a convex (0001) face on which many twin individuals are produced by a two-dimensional nucleation mechanism, resulting in complicated twinning during growth. Both the r and the faces repeat finely during growth because of twinning, resulting in {112̄3} sectors with polysynthetic twinning. Finally, single structures nucleate on the crystal edges [211̄] and develop along the (112̄3) face, penetrating each other near the centre of the face.

Type
Mineralogy
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

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References

Akizuki, M. (1981) Litho. 14, 17-21.CrossRefGoogle Scholar
Akizuki, M. (1985) Am. Mineral. 70, 814-21.Google Scholar
Dana, E.S. (1892) The System of Mineralogy. John Wiley and Sons, Inc. New York.Google Scholar
Gottardi, G. and Galli, E. (1985) Natural Zeolites, Springer-Verlag.CrossRefGoogle Scholar
Lasaulx, A.V. (1881) Z. Kristallogr. 5, 327-47.Google Scholar
Mazzi, F. and Galli, E. (1983) Neues Jahrb. Mineral. Mh. 461-80.Google Scholar
Narita, G. (1968) Graduation thesis, Tohoku University (unpubl.).Google Scholar
Walker, G.P.L. (1951) Mineral. Mag. 29, 773-91.Google Scholar