Genesis of post-hotspot, A-type rhyolite of the Eastern Snake River Plain volcanic field by extreme fractional crystallization of olivine tholeiite

Bulletin of Volcanology

Volumn 70, Issue 3, 2008, Pages 361-383

  McCurry, Michael ^a   Hayden, Karl P ^a   Morse, Lee H ^a   Mertzman, Stan ^b  

^a IDAHO STATE UNIVERSITY   (United States)

^b FRANKLIN AND MARSHALL COLLEGE   (United States)

Author keywords

A type magma; Basalt differentiation; Bimodal volcanism; Fractional crystallization; Hotspot; Rhyolite genesis; Yellowstone Snake river Plain

Indexed keywords

A-TYPE ROCK; ANDESITE; BASALT; FRACTIONAL CRYSTALLIZATION; HOT SPOT; IGNEOUS GEOCHEMISTRY; IGNEOUS INTRUSION; ISOTOPIC COMPOSITION; LAVA; MAGMA; MAGMATIC DIFFERENTIATION; MELTING; OLIVINE; PETROGENESIS; RHYOLITE; SHIELD VOLCANO; THOLEIITE; VOLCANISM;

IDAHO; NORTH AMERICA; SNAKE RIVER PLAIN; UNITED STATES;

EID: 38049160145     PISSN: 02588900     EISSN: 14320819     Source Type: Journal    
DOI: 10.1007/s00445-007-0143-4     Document Type: Article

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