Estudio geológico del campo filoniano de la Fregeneda ( Huelva )

1. Gonzalo, J. C. ¹
2. Carnicero, A. ¹
3. López Plaza, M. 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

×

Non se pode exportar o documento porque pertence a outro portal.

Texto completo

lock_openTexto completo externo

DIALNET GOOGLE SCHOLAR lock_openAcceso aberto editor

Outras publicacións en: Studia geologica salmanticensia

Resumo

In this work a close dike field has been studied. Emphasis is placed on the composition and fundamental properties of these dikes: their conexión with the regional tectonic and granitic rocks and their genesis and emplacement. According to these data, we have distinguished three main groups: N-S pegmatite dikes, WN W-ESE concordant sheets and E-SE zone dikes. Their sequence has been established and is compared with certain theoretical models for magma intrusion (ROBERTS' model).

Fonte de datos: Dialnet