Temporal geochemical evolution of Neogene volcanism in northern Baja California (27°-30° N): Insights on the origin of post-subduction magnesian andesites

Lithos

Volumn 105, Issue 1-2, 2008, Pages 162-180

  Pallares, Carlos ^a,b   Bellon, Hervé ^a   Benoit, Mathieu ^a   Maury, René C ^a   Aguillón Robles, Alfredo ^c   Calmus, Thierry ^b   Cotten, Joseph ^a  

^a INSTITUT UNIVERSITAIRE EUROPÉEN DE LA MER   (France)

^b UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO   (Mexico)

^c UNIVERSIDAD AUTÓNOMA DE SAN LUIS POTOSÍ   (Mexico)

Author keywords

Asthenospheric window; Baja California, M xico; Magnesian andesite; Mantle metasomatism; Slab melting

Indexed keywords

ANDESITE; CALC ALKALINE ROCK; DEHYDRATION MELTING; GARNET; LITHOSPHERIC STRUCTURE; MAGNESIUM; NEOGENE; POTASSIUM-ARGON DATING; RARE EARTH ELEMENT; SUBDUCTION; TEMPORAL EVOLUTION; TRACE ELEMENT; VOLCANISM;

BAJA CALIFORNIA [(PNN) MEXICO]; MEXICO [NORTH AMERICA]; NORTH AMERICA;

EID: 51849089182     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2008.03.004     Document Type: Article

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