Oxygen Isotopic Composition of Coexisting Minerals of Sillimanite-Hypersthene Rocks from the Por'ya Bay Area: Evidence of Fluid Involvement in Granulite-Facies Metamorphism

Geochemistry International

Volumn 48, Issue 8, 2010, Pages 739-751

  Aranovich, L Ya ^a   Dubinina, E O ^a   Avdeenko, A S ^a   Lebedeva, Yu M ^b   Bushmin, S A ^b   Dolivo Dobrovol'skii, D D ^b  

^a INSTITUTE OF GEOLOGY OF ORE DEPOSITS   (Russian Federation)

^b INSTITUTE OF PRECAMBRIAN GEOLOGY AND GEOCHRONOLOGY   (Russian Federation)

Author keywords

[No Author keywords available]

Indexed keywords

BAY AREAS; CHEMICAL COMPOSITIONS; CLINOPYROXENES; COEXISTING MINERALS; FLUID FLUXES; FLUID-ROCK INTERACTION; GEOTHERMOMETERS; GRANULITE FACIES; HIGH TEMPERATURE; ISOTOPIC SYSTEMS; MINERAL ASSEMBLAGE; MINERAL COMPOSITION; MODEL CALCULATIONS; ORTHOPYROXENE; OXYGEN ISOTOPIC; OXYGEN ISOTOPIC COMPOSITION; PROTEROZOIC; PROTOLITHS; QUALITATIVE ANALYSIS; ROCK-FORMING MINERALS; SHEAR ZONE; SYSTEMATIC VARIATION;

FLUIDS; ISOTOPES; OXYGEN; QUARTZ; ROCKS; SILICATE MINERALS;

MINERALS;

GARNET; GRANULITE FACIES; ISOTOPIC COMPOSITION; METAMORPHISM; OXYGEN ISOTOPE; QUARTZ; SHEAR ZONE; SILLIMANITE;

EID: 77956115542     PISSN: 00167029     EISSN: 15561968     Source Type: Journal    
DOI: 10.1134/S001670291008001X     Document Type: Article

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