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[4]Si substitution in natural tourmalines
1 Department of Geology, Miami University, Oxford, Ohio 45056, U.S.A.
2 Department of Geography and Geology, Mount Holyoke College, South Hadley, Massachusetts 01075, U.S.A.
E-mail: hughesjm{at}muohio.edu
* Present address: Civil Engineering and Geological Sciences, Notre Dame, Notre Dame, Indiana 46556, U.S.A.
Because tourmaline is the most common boron-bearing mineral, the crystal chemistry of B in the phase is of fundamental importance to understanding the boron budget in the Earth. Until recently, the presence of [4]B as a substituent in the tourmaline tetrahedral (T) ring was unrecognized. However, a study of an Austrian olenite has shown that the substitution is not only possible but can occur in amounts up to B1.00 per T6.00.
Through Magic-Angle-Spinning Nuclear Magnetic Resonance (MAS-NMR) spectroscopy, it was recently shown that [4]B in tourmaline can be identified by its spectroscopic signature. This study characterizes the structural response to small (< 0.50 apfu) amounts of substituent [4]B. Two tourmaline samples ([4]B.0.028, [4]B0.37 by chemical analysis) that have been demonstrated by MAS-NMR to contain [4]B were analyzed by single-crystal X-ray techniques. It was found that reasonable agreement is obtained between [4]B content as determined by Secondary Ion Mass Spectrometry and X-ray site refinement, although the X-ray refinement significantly overestimates [4]B (by 30) in one sample.
The response of the tourmaline atomic arrangement to the incorporation of substituent [4]B is subtle, perhaps explaining the lack of previous recognition of the substitution. The P-T-X conditions required for the substitution are not known, but are being studied by mineral researchers; it has been observed that all of the [4]B-bearing tourmalines discovered to date contain little or no Mg on the octahedral sites.
Key-words: tourmaline, boron, crystal-structure refinement.
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