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handle: 20.500.14352/42507 , 10261/62067
La importancia del plutón granítico de Logrosán (Cáceres) reside en las mineralizaciones filonianas de Sn-(Ta)-W asociadas a la cúpula granítica, y en los yacimientos peri-graníticos de fosfatos localizados en su aureola de metamorfismo de contacto (Sos Baynat, 1965; Locutura et al., 2006). En este resumen se presenta el estudio textural y metalogenético de las mineralizaciones intragraníticas de Sn- (Ta)-W. Así mismo, se realiza una aproximación a las condiciones de formación del depósito mineral.
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Logrosán granite., 552.3(460.251), Logrosán granite, Química mineral, 553.521(460.251), Mineralogía (Geología), Mineral chemistry, Granito de Logrosán, Ore genesis, Mineralogía, Génesis mineral, 2506.11 Mineralogía
Logrosán granite., 552.3(460.251), Logrosán granite, Química mineral, 553.521(460.251), Mineralogía (Geología), Mineral chemistry, Granito de Logrosán, Ore genesis, Mineralogía, Génesis mineral, 2506.11 Mineralogía
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