Structural and petrologic evolution of the Bear Peak intrusive complex, Klamath Mountains, California

Special Paper of the Geological Society of America

Volumn 410, Issue , 2006, Pages 333-355

  McFadden, Rory R ^a   Snoke, Arthur W ^a   Barnes, Calvin G ^b  

^a UNIVERSITY OF WYOMING   (United States)

^b TEXAS TECH UNIVERSITY   (United States)

Author keywords

Contact metamorphism; Enclaves; Galice formation; Jurassic; Migmatitic amphibolite; Oceanic arc pluton; Rattlesnake creek terrane; Siskiyou mountains; Ultramafic rocks

Indexed keywords

BASALT; EXPLORATORY GEOCHEMISTRY; LANDFORMS; MAGNESITE; MELTING; METAMORPHIC ROCKS; MICA; QUARTZ; RARE EARTHS; SEDIMENTARY ROCKS; SILICATE MINERALS;

CONTACT METAMORPHISM; ENCLAVES; GALICE FORMATION; JURASSIC; MIGMATITIC AMPHIBOLITE; OCEANIC-ARC PLUTON; RATTLESNAKE CREEK TERRANE; SISKIYOU MOUNTAINS; ULTRAMAFIC ROCKS;

FAULTING;

AMPHIBOLITE; ANDALUSITE; CLINOPYROXENE; CONTACT METAMORPHISM; DIKE; DIORITE; GABBRO; GREENSCHIST FACIES; HORNBLENDE; HOST ROCK; JURASSIC; LOW GRADE METAMORPHISM; METAMORPHISM; MIGMATIZATION; OROGENY; PARTIAL MELTING; PETROLOGY; PLUTON; TECTONIC EVOLUTION; TERRANE; THRUST FAULT; ULTRAMAFIC ROCK;

COAST RANGES; KLAMATH MOUNTAINS; SISKIYOU MOUNTAINS; UNITED STATES;

EID: 73949101848     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2006.2410(16)     Document Type: Article

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