Volatile contents of mafic magmas from cinder cones in the Central Oregon High Cascades: Implications for magma formation and mantle conditions in a hot arc

Earth and Planetary Science Letters

Volumn 298, Issue 1-2, 2010, Pages 153-161

  Ruscitto, D M ^a   Wallace, P J ^a   Johnson, E R ^a,c   Kent, A J R ^b   Bindeman, I N ^a  

^a UNIVERSITY OF OREGON   (United States)

^b OREGON STATE UNIVERSITY   (United States)

^c UNIVERSITY OF TASMANIA   (Australia)

Author keywords

Cascades; Melt inclusions; Subduction zones; Volatiles

Indexed keywords

ARC SPECTRUM; BASALTIC ANDESITE; BASALTIC MELTS; CASCADES; CASCADES ARC; CENTRAL AMERICA; FOREARC; INCLUSION COMPOSITION; INCOMPATIBLE ELEMENT; KAMCHATKA; MAGMATIC VOLATILES; MANTLE SOURCE; MANTLE WEDGE; ME-XICO; MELT INCLUSIONS; OCEANIC CRUST; PARTIAL MELTING; POSITIVE CORRELATIONS; SLAB TEMPERATURE; SPINEL-LHERZOLITE; SUB-ARC MANTLE; SUBDUCTING SLABS; SUBDUCTION ZONES; SURFACE TEMPERATURES; VOLATILE ABUNDANCES; VOLATILE CONTENTS; VOLATILES;

BASALT; FORESTRY; IGNEOUS ROCKS; OLIVINE; SILICATE MINERALS; SPECTROSCOPY; TECTONICS; TRACE ELEMENTS;

INCLUSIONS;

CALC ALKALINE ROCK; CINDER CONE; CRYSTALLIZATION; DEGASSING; MAFIC ROCK; MAGMA; MELT INCLUSION; MID-OCEAN RIDGE BASALT; OCEANIC CRUST; SUBDUCTION ZONE; VOLATILE SUBSTANCE;

CASCADE RANGE; OREGON; UNITED STATES;

EID: 77957255916     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2010.07.037     Document Type: Article

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