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handle: 10261/36402
[ESP] Los granitos cordieriticos del área estudiada se interpretan como productos infracorticales hibridados con material de la corteza, emplazándose según fallas antiguas de importancia regional. La cxistencia de diques básicos apoya la idea de fracturaciones importantes a nivel cortical, que han sido las canales para la inyección de los Ruidos alcalinos de origen profundo. generadores de la rubefacción granitica.
[ENG] The granites around Linares de Riofrio-Bejar are interpreted as of deep origin, generated by fusion of continental crust and melange with a infracrustal material: the magma roses across older deep-seated fault. Red granites are products of alkaline metasomatism by deep level fluids.
13 p.
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