The Canadian Mineralogist; June 2007; v. 45; no. 3;
p. 541-549; DOI: 10.2113/gscanmin.45.3.541
© 2007 Mineralogical Association of Canada
UNUSUAL FIBROUS SODIAN TAINIOLITE EPITACTIC ON PHLOGOPITE FROM MARBLE XENOLITHS OF MONT SAINT-HILAIRE, QUEBEC, CANADA
Thomas Armbruster1,
,
R. Peter Richards2,
Edwin Gnos3,
Thomas Pettke3 and
Marco Herwegh3
1 Laboratorium für chemische und mineralogische Kristallographie, Universität Bern, Freiestr. 3, CH–3012 Bern, Switzerland
2 National Center for Water Quality Research, Heidelberg College, Tiffin, Ohio 44883, USA
3 Institut für Geologie, Universität Bern, Balzerstr. 1, CH–3012 Bern, Switzerland

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FIG. 2. Paragenesis (early: left, late: right) of the minerals associated with the phlogopite with tainiolite overgrown.
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FIG. 3. Polyhedral representation of a trioctahedral mica structure, 1M polytype (space group C2/m), projected perpendicular to (001). Growth fronts (traces of crystal faces) are indicated by dashed white lines, unit-cell outlines are shown by solid black lines. Magenta spheres represent interlayer K, decorating the (010) growth surface. In tainiolite, growth of this surface is retarded due to "poisoning".
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Copyright © 2008 by Mineralogical Association of Canada