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http://hdl.handle.net/2183/5923 Caracterización geoquímica del complejo plutónico de Taliga-Barcarrota (Badajoz, España)
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Galindo, C.
Casquet Martín, César
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Cadernos do Laboratorio Xeolóxico de Laxe, 1985, 9: 49-62 ISBN: 84-7492-367-4
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Abstract
[Resumen] En el Complejo Plutónico de Táliga-Barcarrota se distinguen dos tendencias geoquimicas: la primera de ellas corresponde a una "asociación peralumínica" representada por los granitos biotíticos de Táliga, la segunda de caracter "cafémico-subalcalino" está constituida por rocas de tipo básico e intermedio del macizo de Barcarrota
[Abstract] In the Plutonic Táliga-Barcarrota Complex two geochemical tendences can be differenciated: the first one corresponds to "peraluminical assoeiation" represented by biotite granites of Táliga, the second one with a "cafemic-subalkaline"character is constituted by basic and intermediate type of the massif of Bacarrota
[Abstract] In the Plutonic Táliga-Barcarrota Complex two geochemical tendences can be differenciated: the first one corresponds to "peraluminical assoeiation" represented by biotite granites of Táliga, the second one with a "cafemic-subalkaline"character is constituted by basic and intermediate type of the massif of Bacarrota