La serie volcánica submarina del Complejo Basal de Fuerteventuracrecimiento submarino y emersión de la Isla

1. Gutiérrez, M.
2. Casillas Ruiz, Ramón
3. Balogh, K.
4. Ahijado Quintillán, Agustina
5. Castillo Ruiz, Carolina

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_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

Resumen

Three lithological units have been distinguished in the volcanic succession of the Basal Complex of Fuerteventura Island, from bottom to top: the Submarine Volcanic Croup, the Transitional Volcanic Croup and the Subaerial Volcanic Croup. These units record the submarine growth and the emersion of the Island. During these stages the volcanism is represented by an ultraalkaline and a strongly alkaline igneous series. The igneous activity was due to the presence of an anomalous zone in the sublithospheric mantle and influenced by the Cenozoic tectonic evolution of the northwestern part of the African plate

Fuente de los datos: Dialnet