Caracterización del plutón granodiorítico de Los Pedroches en su sector noroccidental (Comarca de La Serena, Badajoz).

1. Alonso Olazabal, A. ¹
2. Carracedo, M. ¹
3. Larrea, F.J. ¹
4. Aranguren, A. ¹

Exportar

Exportar

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Exportar

×

El documento no se puede exportar porque pertenece a otro portal.

Texto completo

lock_openTexto completo externo

DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Geogaceta

Resumen

This paper is a brief description of the Hercynian calc-alkaline granodioritic pluton of the Los Pedroches batholith at its NW branch (La Serena, Badajoz). This study is located in the National Topographic Map N.T.M. number 805 of Castuera, and it takes into account only the plutonic rocks. Three main lithotypes have been recognized through field, petrological and geochemical studies: biotitic granodiorite±amphibole, piroxenic granodiorite and Las Cabezas granite. Whole chemistry defines a potassium-rich, aluminic-cafemic calcalkaline magmatic association.

Fuente de los datos: Dialnet