Abstract
A veinlet croscutting the host granulite foliation in the Bory Granulite Massif contains mineral assemblage involving grandidierite-ominelite, boralsilite, Fe-analogue of werdingite, dumortierite (locally Sb,Ti-rich), tourmaline and corundum. The assemblage formed at medium pressure and moderate temperature during the exhumation of the granulite body.
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Schedule a callMore From: American Mineralogist: Journal of Earth and Planetary Materials
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