Granitoides peraluminosos y su relación con las rocas fuentes
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Publication date
2005
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Sociedad Geológica de España
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Abstract
Comparative compositional studies between two peraluminous unit with magmatic andalucite and cordierite
indicate that they were produced by partial melting of two differents metasedimentary source rocks. We
conclude that geochemical studies from peraluminous unit contributes to define the source rocks and to
constrain the pre-orogenic geotectonic environment