| Registros del 1 al 4 de 4 encontrados |
1.- Adakitic dacites formed by intracrustal crystal fractionation of water-rich parent magmas at Nevado de Longavi Volcano (36.2 degrees S; Andean southern volcanic zone, central Chile)
Oxford University Press; Oxford; GBR; United Kingdom, 2007
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2.- Correlated oxygen fugacity and slab-derived fluid flux linked to oceanic fracture zone subduction at Nevado de Longavi Volcano, Southern Andes
American Geophysical Union; Washington, DC; USA; United States, 2005
AGU 2005 fall meeting
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3.- EVOLUTION OF THE LATE PALEOZOIC ACCRETIONARY COMPLEX AND OVERLYING FOREARC-MAGMATIC ARC, SOUTH CENTRAL CHILE (38 DEGREES -41 DEGREES S); CONSTRAINTS FOR THE TECTONIC SETTING ALONG THE SOUTHWESTERN MARGIN OF GONDWANA
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1999
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4.- Nevado de Longavi dacites; adakite genesis by intra-crustal fractional crystallization in a cold subduction zone
American Geophysical Union; Washington, DC; USA; United States, 2005
AGU 2005 fall meeting
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