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- W2137185400 abstract "Servicio Nacional de Geologia y Mineria, SERNAGEOMIN, Santiago, (hileIntroductionAdakitic-like rocks are andesitic to dacitic hydrous magmas that exhibit fractionated REE patterns (highLa/Yb) consistent with gamet involvement as weil as evidence for Jackof plagioclase in the residual assemblage(high Sr, no Eu anomaly). Compared to normal evolved arc magmas, adakitic rocks tend to have slightly highercontents of compatible elements (Mg, Cr, Ni), but have similar or lower concentrations of incompatibleelements. Adakite-like magmas in arcs are often interpreted as melts derived from crustal sources (oceanic orcontinental) that have either reacted with the mantle wedge or interacted with primitive arc basaltic magmas.There is general agreement that, to produce adakitic melts, the crustal sources involved must be mafic (basaltic)in composition and at a depth within the stability field ofgarnet. In general, it is difficult to identify the oceanicor continental nature of the source involved, as it is to explain the very local occurrence, both in space and time,of adakitic magmatism within voJcanic arcs. An alternative process to explain adakitic magmas by crystalfractionation (Kleinhanns" @default.
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- W2137185400 date "2005-01-01" @default.
- W2137185400 modified "2023-09-26" @default.
- W2137185400 title "Garnet phenocrysts in early miocene intrusives in central Chile : evidence for a crystal fractionation origin of adakite-like magmas" @default.
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