Granulite- to amphibolite-facies metamorphism and penetrative deformation in a disrupted ophiolite, Klamath Mountains, California: A deep view into the basement of an accreted oceanic arc

Special Paper of the Geological Society of America

Volumn 456, Issue , 2009, Pages 151-186

  Garlick, Sarah R ^a   Medaris, L Gordon ^b   Snoke, Arthur W ^a   Schwartz, Joshua J ^a   Swapp, Susan M ^a  

^a UNIVERSITY OF WYOMING   (United States)

^b UNIVERSITY OF WISCONSIN MADISON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BINARY ALLOYS; BUILDINGS; FAULTING; GEOCHRONOLOGY; LANDFORMS; LEAD ALLOYS; SEDIMENTARY ROCKS; STRUCTURAL GEOLOGY; URANIUM ALLOYS; ZIRCON;

AMPHIBOLITE-FACIES METAMORPHISM; CALIFORNIA; CONDITION; CRUSTALS; GRANULITE FACIES; ISLAND ARC; MESOZOIC; NEO GENES; OCEANIC CRUST; TECTONIC SLICES;

DEFORMATION;

ACCRETION; AMPHIBOLITE FACIES; DEFORMATION MECHANISM; GRANULITE FACIES; HIGH TEMPERATURE; ISLAND ARC; MELANGE; MESOZOIC; METAGABBRO; METAMORPHISM; OCEANIC CRUST; OPHIOLITE; P-T CONDITIONS; TECTONIC EVOLUTION; TECTONIC SETTING; TERRANE; URANIUM-LEAD DATING; ZIRCON;

CALIFORNIA; COAST RANGES; KLAMATH MOUNTAINS; UNITED STATES;

EID: 74949093052     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2009.2456(06)     Document Type: Article

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