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European Journal of Mineralogy; March, April 2004; v. 16; no. 2; p. 335-344; DOI: 10.1127/0935-1221/2004/0016-0335
© 2004 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Crystal chemistry of the schorl-dravite series

Ferdinando BOSI and Sergio LUCCHESI*

Dipartimento di Scienze della Terra, Università di Roma "La Sapienza", P.le A. Moro 5, 1–00186 Roma, Italy

* E-mail: sergio.lucchesi{at}uniromal.it

Nineteen tourmaline samples of various provenances and geological settings were studied by EMPA, SREF and MS to represent the schorl-dravite compositional field. All samples belong to the Alkali group (except one with an X-site vacancy content of 0.53 apfu) and to the Oxy- and Hydroxy-subgroups. Among divalent cations, the main substitution involves YMg for YFe2+, to produce the two end-members dravite and schorl.

Site populations were determined by a new minimization procedure that simultaneously accounts for both structural and chemical data. Results show that the crystals are characterized by disordered cation distribution between Y and Z sites: Al populates both sites, with a marked preference for the smaller Z octahedron; Mg is often equally distributed between Y and Z. Both Fe2+ and Fe3+ populate both Y and Z sites, but show a strong preference for Y. Specific mean bond distances (Å) optimised for major elements are: YAl-O = 1.908, YMg-O = 2.084, YFe2+-O = 2.139, zAl-O = 1.900, zMg-O = 2.077 and zFe2+-O = 2.131.

In the schorl-dravite solid solution, structural variations appear to be primarily due to Y and Z interactions. These effects are conspicuous over the entire structure, as Y dimensions directly affect the a cell parameter, while Z is similarly correlated with c. The dimensions of Y and Z octahedra are determined by Al contents. Dimensional variations of Z are well described by its bond-distance variations, except for Z-07D. Both octahedra reciprocally interact, influencing their distortions: inverse correlations exist between Y dimension vs. Z quadratic elongation and Z dimension vs. Y quadratic elongation. As a common feature, the effects of the octahedral second coordination sphere are only confined to polyhedral distortions instead of dimensional variations, which only depend on site populations.

Key-words: Crystal structure, crystal-chemistry, disorder, schorl, dravite, tourmaline.




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