Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism.

Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism.

Aranovich, L Ya; Dubinina, E O; Avdeenko, A S; Lebedeva, YuM; Bushmin, S A; Dolivo-Dobrovol'skii, D D
xmlui.dri2xhtml.METS-1.0.item-citation: Aranovich, L Ya; Dubinina, E O; Avdeenko, A S; Lebedeva, YuM; Bushmin, S A; Dolivo-Dobrovol'skii, D D (2010): Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism. Translated from Geokhimiya, 2010, 48(8), 787-800, Geochemistry International, 48(8), 739-751, https://doi.org/10.1134/S001670291008001X
Date: 2010-08-03

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