| Registros del 1 al 5 de 5 encontrados |
1.- Extreme high field strength element (HFSE) depletion and near-chondritic Nb/Ta ratios in Central Andean adakite-like lavas ( approximately 28 degrees S, approximately 68 degrees W)
Elsevier; Amsterdam; NLD; Netherlands, 2009
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2.- Neogene Central Andean adakites, frontal arc migration and forearc subduction erosion at 27 degrees -28.5 degrees S
Mineralogical Society; London; GBR; United Kingdom, 2011
Goldschmidt 2011 abstract volume
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3.- Steep REE patterns and enriched Pb isotopes in southern Central American arc magmas; evidence for forearc subduction erosion?
American Geophysical Union and The Geochemical Society;; USA; United States, 2006
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4.- The geochemistry of a dying continental arc; the Incapillo Caldera and dome complex of the southernmost Central Andean volcanic zone ( approximately 28 degrees S)
Springer International; Heidelberg - New York; III; International, 2011
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5.- The Incapillo Caldera; a stranded magma chamber over a dying Andean arc
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
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