Boron in Sillimanite
Document Type
Article
Department or Administrative Unit
Geological Sciences
Publication Date
8-5-1983
Abstract
Sillimanite in six granulite-facies, kornerupine-bearing rocks contains 0.035 to 0.43 percent B2O3 and 0.02 to 0.23 percent MgO (by weight). Substitution of boron for silicon and magnesium for aluminum is coupled such that the ratio of magnesium to boron is about 0.5. Sillimanite incorporates more than 0.1 percent B2O3 only at high temperatures in a boron-rich environment at very low partial pressures of water. In the amphibolite facies, the sillimanite boron contents are too low to appreciably affect the stability relations of sillimanite with kyanite and andalusite.
Recommended Citation
Grew, E. S., & Hinthorne, J. R. (1983). Boron in Sillimanite. Science, 221(4610), 547–549. https://doi.org/10.1126/science.221.4610.547
Journal
Science
Rights
Copyright © 1983 by the American Association for the Advancement of Science.
Comments
This article was originally published in Science. The full-text article from the publisher can be found here.
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