Caracterización geoquímica del complejo plutónico de Taliga-Barcarrota (Badajoz, España)
Loading...
Download
Official URL
Full text at PDC
Publication date
1985
Advisors (or tutors)
Editors
Journal Title
Journal ISSN
Volume Title
Publisher
Seminario de Estudos Galegos. Area de Xeoloxía e Minería ; Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
Citations
Exportar
Citation
Abstract
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.
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 basie and intermediate type of the massif of Barcarrota.
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 basie and intermediate type of the massif of Barcarrota.