Evolving metasomatic agent in the Northern Andean subduction zone, deduced from magma composition of the long-lived Pichincha volcanic complex (Ecuador)

Contributions to Mineralogy and Petrology

Volumn 160, Issue 2, 2010, Pages 239-260

  Samaniego, Pablo ^a,b,c,d   Robin, Claude ^c,d   Chazot, Gilles ^e,f   Bourdon, Erwan ^g   Cotten, Joseph ^e,f  

^a UNIVERSITÉ CLERMONT AUVERGNE   (France)

^b CNRS   (France)

^c UNIVERSITÉ BLAISE PASCAL   (France)

^d ESCUELA POLITÉCNICA NACIONAL   (Ecuador)

^e UNIVERSITÉ EUROPÉENNE DE BRETAGNE   (France)

^f INSTITUT UNIVERSITAIRE EUROPÉEN DE LA MER   (France)

^g Route de l'Observatoire Le Houëlmont ^*  (Guadeloupe)

Author keywords

Adakite; Arc magmatism; Ecuador; Isotopes; Northern Andean Volcanic Zone; Pichincha; Subduction; Trace elements

Indexed keywords

ADAKITE; ANDESITE; FRACTIONAL CRYSTALLIZATION; GEOTHERMAL GRADIENT; ISOTOPIC COMPOSITION; MAGMATISM; MANTLE SOURCE; METASOMATISM; PARTIAL MELTING; SUBDUCTION ZONE; TRACE ELEMENT;

CARNEGIE RIDGE; ECUADOR; PACIFIC OCEAN; PICHINCHA;

EID: 77954426006     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-009-0475-5     Document Type: Article

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