Metamorphic evolution of sapphirine- and orthoamphibole-cordierite-bearing gneiss, Okanogan dome, Washington, USA

Journal of Metamorphic Geology

Volumn 29, Issue 4, 2011, Pages 425-449

  Kruckenberg, S C ^a   Whitney, D L ^b  

^a UNIVERSITY OF MINNESOTA   (United States)

^b UNIVERSITY OF WISCONSIN MADISON   (United States)

Author keywords

High temperature metamorphism; Mg Al gneiss; North American Cordillera; Okanogan dome; Omineca belt; Orthoamphibole cordierite; Pseudosection; Reaction textures; Sapphirine spinel; Symplectite; Washington

Indexed keywords

HIGH TEMPERATURE; MG-AL GNEISS; NORTH AMERICAN CORDILLERA; OKANOGAN DOME; OMINECA BELT; ORTHOAMPHIBOLE-CORDIERITE; PSEUDOSECTION; REACTION TEXTURES; SAPPHIRINE-SPINEL; SYMPLECTITE; WASHINGTON;

ALUMINUM; DOMES; MICA; PHASE EQUILIBRIA; REFRACTORY MATERIALS; ROCKS; SILICATE MINERALS; TECTONICS; TEXTURES;

METAMORPHIC ROCKS;

AMPHIBOLE; CORDIERITE; DECOMPRESSION; ORTHOGNEISS; P-T CONDITIONS; P-T-T PATH; PETROGRAPHY; SAPPHIRINE; SPINEL; SYMPLECTITE; TECTONIC EVOLUTION; TECTONIC SETTING; TEXTURE; ULTRAHIGH TEMPERATURE METAMORPHISM;

NORTH AMERICAN CORDILLERA; OKANOGAN DOME; OMINECA BELT; UNITED STATES; WASHINGTON [UNITED STATES];

EID: 79953268561     PISSN: 02634929     EISSN: 15251314     Source Type: Journal    
DOI: 10.1111/j.1525-1314.2010.00926.x     Document Type: Article

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