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American Mineralogist; July 2007; v. 92; no. 7; p. 1054-1063; DOI: 10.2138/am.2007.2370
© 2007 Mineralogical Society of America
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Crystal chemical relationships in the tourmaline group: Structural constraints on chemical variability

Ferdinando Bosi1,* and Sergio Lucchesi2

1 Department of Mineralogy, Swedish Museum of Natural History, Box 50007, 10405 Stockholm, Sweden
2 Dipartimento di Scienze della Terra, Università degli Studi di Roma "La Sapienza," P.le A. Moro 5, 00185 Roma, Italy

Correspondence: * E-mail: ferdinando.bosi{at}uniroma1.it

This paper explores some aspects of the crystal chemistry and structural constraints on tourmaline by examining 127 samples from the literature. According to the bond-valence model, the tourmaline structure shows lattice-induced strain at each polyhedron. The overall effect is an expansion of the triangular (BO3) group and compression of the tetrahedron. The X polyhedron can be either compressed or expanded: compression increases with vacancy content, whereas expansion is typical of Ca-rich tourmaline. The Y octahedron changes extensively from compressed through an unstrained to expanded state as a function of increasing Li content. The Z octahedron is almost unstrained in crystals with {sum}ZR2+ < 0.40 apfu, whereas it is compressed in crystals with {sum}ZR2+ > 0.40 apfu.

The configuration of the six-membered tetrahedral ring is strongly affected by <Y-O>, which is the most important parameter linked to the deviation of the tetrahedral ring from hexagonal symmetry. The whole structure is stable when the channels through the Z octahedron framework are able to accommodate the Y cations. As <Y-O> becomes larger, the less puckered the tetrahedral ring and the more the O7 atom is displaced away from Z. Consequently, the difference between <Y-O> and <Z-O> cannot be too large, otherwise <Z-O> will be too small to be commensurate with shifting of the O7 atom. One possible mechanism to reduce the difference between <Y-O> and <Z-O>, is the disordering reaction YAl + ZR -> YR + ZAl, which increases <Z-O> and decreases <Y-O>. In ideal dravite, schorl, and "tsilaisite," <Y-O> and <Z-O> are incommensurate.

Key Words: Order-disorder • crystal structure • tourmalina • XRD data




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Linking Mossbauer and structural parameters in elbaite-schorl-dravite tourmalines
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