El Aptiense de Lanestosa (Bizkaia)implicaciones palotectónicas

1. López-Horgue, M.A
2. Fernández-Mendiola, P.A
3. García-Mondéjar, J.

Exporter

Exporter

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Exporter

×

Le document ne peut pas être exporté car il appartient à un autre portail.

Texte intégral

lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

D'autres publications dans: Geogaceta

Résumé

The Aptian of Lanestosa is analyzed based on detailed mapping and facies analysis. Four sedimentary units are differentiated: a basal terrigenous unit and three overlying carbonate platform units. Units boundaries 2-3 and 3-4 represent unconformity surfaces linked to synsedimentary tectonic activity. The Cabuerniga-Ramales E-W trending fault is responsible of the repeated block tilting in mid Aptian and late Aptian times. The origin of Pb-Zn ores in this area is likely related to this tectonic activity

La source de données: Dialnet