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Abstract

Dark brown crystals, up to 10 mm long, occur in rhyolite at Mexquitic, San Luis Potosi, Mexico. They are short prismatic, showing {112̅0}, {303̅0}, {101̅1}, {022̅1}, with c/a 0.4521, measured with a goniometer, and distinct {112̅0} cleavage. With an unusual combination of cell dimensions, high density, high refractive indices, and extreme birefringence, this tourmaline falls outside the known elbaite-schorl and schorl-dravite series. A chemical analysis, recalculated on the basis of cell volume and density, gives close to the theoretical 150 atoms per cell, whether the iron is ferrous or ferric, but the physical properties indicate a ferric tourmaline.

References

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Published In

Science
Volume 144 | Issue 3614
3 April 1964

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Published in print: 3 April 1964

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Brian Mason
American Museum of Natural History, New York 24
Gabrielle Donnay
Geophysical Laboratory, Carnegie Institution of Washington, Washington, D. C.
L. A. Hardie
Johns Hopkins University, Baltimore, Maryland

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