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Nanometre scale textures in agate and Beltane opal

Published online by Cambridge University Press:  05 July 2018

Taijing Lu ,
X. Zhang ,
Ichiro Sunagawa  and
G. W. Groves
Taijing Lu
Affiliation:
Department of Physics, National University of Singapore, Lower Kent Ridge Road, Singapore 0511
X. Zhang
Affiliation:
Department of Physics, National University of Singapore, Lower Kent Ridge Road, Singapore 0511
Ichiro Sunagawa
Affiliation:
Yamanashi Institute of Gemology and Jewelry Arts, Tokoji-machi, 1955-1, Kofu, Yamanashi, 400 Japan
G. W. Groves
Affiliation:
Department of Materials, University of Oxford, Parks Road, Oxford OX1 3PH, UK
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Abstract

We have carried out TEM observations of agates of geode origin and Beltane opals. Optically observable individual fibres in agates are composed of many fine fibres which consist of quartz crystallites of 8 to 100 nm in length stacked together parallel to <110> or <100> with c-axes perpendicular to the fibre elongation. The optically observable systematic striations in agate are found to consist of cyclic alternation of layers due to variation in grain size and porosity. Large quartz crystals, protruding into the spaces of geodes, represent the last stage of formation of these bands, and are merely a continuation of the banding sequence. Nanometre scale textures of cristobalite fibres were revealed in Beltane opals. The cristobalite crystallites have the size of 3 to 20 nm in length and are also stacked together. Our TEM results suggest that embryonic particles were formed in their corresponding growth environments and agglutinated to form fibres.

Keywords

agateopaltextureTEM observationfibre
Type
Mineralogy
Information
Mineralogical Magazine , Volume 59 , Issue 394 , March 1995 , pp. 103 - 109
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1995

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References

Ball, R. A. and Bums, R. L. (1975) Austral Gemol., 12, 143–50.Google Scholar
Braitsch, O. Y. (1957) Beitr. Mineral. Petrogr., 5, 331-72.Google Scholar
Brewster, D. (1843) Philos. Mag., 22, 434–5.Google Scholar
Copisarow, A. C. and Copisarow, M. (1942) Nature, 149, 413.CrossRefGoogle Scholar
Correns, C. W. and Nagelschmidt, G. (1933) Zeits. Kristallogr., 85, 199–213.Google Scholar
Frondel, C. (1962) The System of Mineralogy, Vol. Ill, Silica Minerals. Seventh Edition, New York, Wiley.Google Scholar
Frondel, C. (1978) Amer. Mineral, 63, 17–27.Google Scholar
Graetsch, H., Florke, O. W. and Miehe G. (1987) Phys. Chem. Minerals, 14, 247–9.CrossRefGoogle Scholar
Groves, G. W., Hodges, D. J. and Zhang, X. (1987) Proc. 9th Intern. Conf. on Cement Microscopy, Reno, USA, 458-65.Google Scholar
Liesegang, R. E. (1915) Die Achate, Dresden Ce, Leipzig (Th. Steinkopff).CrossRefGoogle Scholar
Taijing, Lu and Sunagawa, I. (1994) Mineral J., 17, 53–76.CrossRefGoogle Scholar
Miehe, G., Graetsh, H. and Florke, O. W. (1984) Phys. Chem. Minerals, 10, 197–9.CrossRefGoogle Scholar
Sunagawa, I. and Ohta, E. (1976) Sci. Rep., Tohoku Univ., 13, 131–46.Google Scholar
Zhang, X., Blackwell, B. Q. and Groves, G. W. (1990) Brit. Ceram. Trans. J., 89, 899–92.Google Scholar