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Structural Data for Sudoite

Published online by Cambridge University Press:  02 April 2024

Cheng-yi Lin  and
S. W. Bailey
Cheng-yi Lin*
Affiliation:
Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706
S. W. Bailey
Affiliation:
Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706
*
1Present address: Center of Materials Analysis, Nanjing University, China.
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Abstract

Single crystals of sudoite from Ottré, Belgium, allow confirmation of a dioctahedral 2:1 layer and a trioctahedral interlayer in a IIb arrangement. A regular 2-layer s structure is formed in which the octahedral stagger within both 2:1 layers is directed along X1 and adjacent layers are alternately displaced by a2/3 and a3/3. Poor quality crystals and twinning prevented three-dimensional refinement. One-dimensional refinement suggests that the smaller d(001) value of dioctahedral chlorites relative to trioctahedral species is due primarily to the thinner dioctahedral sheet.

Keywords

ChloriteCrystal structureSudoiteSymmetryVermiculite
Type
Research Article
Information
Clays and Clay Minerals , Volume 33 , Issue 5 , October 1985 , pp. 410 - 414
Copyright
Copyright © 1985, The Clay Minerals Society

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References

Aleksandrova, V. A., Drits, V. A. and Sokolova, G. V., 1972 Structural features of dioctahedral one-packet chlorite Soviet Phys. Crystallogr. 17 456–461.Google Scholar
Bailey, S. W. and Brown, B. E., 1962 Chlorite polytypism: I. Regular and semi-random one-layer structures Amer. Mineral. 47 819–850.Google Scholar
Busing, W. R., Martin, K. O., and Levy, H. A. (1962) ORFLS, a Fortran crystallographic least-squares program: Oak Ridge National Laboratory Tech. Manual 305, 75 pp.Google Scholar
de la Calle, C., Dubemat, J., Suquet, H., Pezerat, H., Gaultier, J., Mamy, J. and Bailey, S. W., 1976 Crystal structure of two-layer Mg-vermiculites and Na,Ca-vermiculites Proc. Int. Clay Conf., Mexico City, 1975 Illinois Applied Publishing, Wilmette 201–209.Google Scholar
Drits, V. A. and Lazarenko, E. K., 1967 The structural and mineralogical character of donbassites Mineralog. Sbornik (L’vovsk. Geol. Obshchestvo) 21 40–48.Google Scholar
Eggleton, R. A. and Bailey, S. W., 1967 Structural aspects of dioctahedral chlorite Amer. Mineral. 52 673–689.Google Scholar
Fransolet, A.-M. and Bourguignon, P., 1978 Di/trioctahedral chlorite in quartz veins from the Ardenne, Belgium Can. Mineral. 16 365–373.Google Scholar
Fransolet, A.-M. and Schreyer, W., 1984 Sudoite, di/trioctahedral chlorite: a stable low-temperature phase in the system MgO-Al2O3-SiO2-H2O Contrib. Mineral. Petrol. 86 409–417.CrossRefGoogle Scholar
Kramm, U., 1980 Sudoite in low-grade metamorphic manganese-rich assemblages N. Jb. Mineral. Abh. 138 1–13.Google Scholar
Mathieson, A Mcl and Walker, G. F., 1954 Crystal structure of magnesium-vermiculite Amer. Mineral. 39 231–255.Google Scholar
North, A. C. T., Phillips, D. C. and Mathews, F. S., 1968 A semi-empirical method of absorption correction Acta Crystallogr. A24 351–359.CrossRefGoogle Scholar
Shirozu, H., 1980 Cation distribution, sheet thickness, and O-OH space in trioctahedral chlorites—an X-ray and infrared study Mineral J. (Japan) 10 14–34.CrossRefGoogle Scholar
Shirozu, H. and Bailey, S. W., 1966 Crystal structure of a two-layer Mg-vermiculite Amer. Mineral. 51 1124–1143.Google Scholar
Shirozu, H. and Higashi, S., 1976 Structural investigations of sudoite and regularly interstratified sericite/sudoite Mineral. J. (Japan) 8 158–170.CrossRefGoogle Scholar