Formation of hybrid arc andesites beneath thick continental crust

Earth and Planetary Science Letters

Volumn 303, Issue 3-4, 2011, Pages 337-347

  Straub, Susanne M ^a,b   Gomez Tuena, Arturo ^c   Stuart, Finlay M ^d   Zellmer, Georg F ^b   Espinasa Perena, Ramon ^c   Cai, Yue ^a,e   Iizuka, Yoshiyuki ^b  

^a Department of Earth and Environmental Sciences   (United States)

^b INSTITUTE OF EARTH SCIENCES   (Taiwan)

^c UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO   (Mexico)

^d SCOTTISH UNIVERSITIES ENVIRONMENTAL RESEARCH CENTRE   (United Kingdom)

^e Och Spine at New York Presbyterian Hospitals   (United States)

Author keywords

Andesite formation; Helium isotopes; High Ni olivine; Mexican Volcanic Belt

Indexed keywords

ANDESITE FORMATION; ANDESITE MELT; ARC MAGMAS; CENTRAL MEXICAN VOLCANIC BELTS; CHEMICAL EVIDENCES; CONTINENTAL CRUSTS; CONVERGENT MARGIN; FRACTIONAL CRYSTALLIZATION; HELIUM ISOTOPES; HIGH-NI OLIVINE; MAGMATISMS; MAJOR ELEMENTS; MANTLE MAGMAS; MANTLE MELT; MELT MIXING; MINOR COMPONENTS; MIXING MODELS; PARTIAL MELT; PETROGENESIS; PLUTONIC ROCKS; STRONG CORRELATION; SUB-ARC MANTLE; SUBDUCTING SLABS; SUBDUCTION ZONES; VOLCANIC BELT;

BASALT; HELIUM; IRON OXIDES; ISOTOPES; OLIVINE; PARAFFIN WAXES; SILICA; SILICATE MINERALS; TECTONICS; VOLCANOES;

IGNEOUS ROCKS;

ANDESITE; COMPUTER SIMULATION; CONTINENTAL CRUST; CONVERGENT MARGIN; EMPLACEMENT; FORMATION MECHANISM; FRACTIONAL CRYSTALLIZATION; HELIUM ISOTOPE; ISOTOPIC RATIO; MAGMATISM; MANTLE SOURCE; NUMERICAL MODEL; PARTIAL MELTING; PETROGENESIS;

MEXICO [NORTH AMERICA]; TRANS-MEXICAN VOLCANIC BELT;

EID: 79952106519     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2011.01.013     Document Type: Article

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