The origin of high-Mg magmas in Mt Shasta and Medicine Lake volcanoes, Cascade Arc (California): Higher and lower than mantle oxygen isotope signatures attributed to current and past subduction

Contributions to Mineralogy and Petrology

Volumn 162, Issue 5, 2011, Pages 945-960

  Martin, E ^a,b   Bindeman, I ^a   Grove, T L ^c  

^a UNIVERSITY OF OREGON   (United States)

^b Sorbonne Universités   (France)

^c MASSACHUSETTS INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

Cascades; Flux melting; Mantle wedge; Oxygen isotopes; Subduction

Indexed keywords

CRUSTAL STRUCTURE; ISOTOPIC COMPOSITION; LAVA; MAGMA; MAGNESIUM; MANTLE CHEMISTRY; MANTLE SOURCE; MANTLE STRUCTURE; OLIVINE; ORTHOPYROXENE; OXYGEN ISOTOPE; PARTIAL MELTING; PHENOCRYST; SUBDUCTION ZONE;

CALIFORNIA; CASCADE RANGE; MEDICINE LAKE VOLCANO; MOUNT SHASTA; UNITED STATES;

EID: 85027917234     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-011-0633-4     Document Type: Article

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