El cabalgamiento de Valdesotosconsecuencias de la acomodación del acortamiento cenozoico en el zócalo del Sistema Central

1. A. Olaiz ¹
2. G. de Vicente ¹
3. R. Vegas ¹
4. J.M. González Casado ²
5. A. Muñoz Martín ¹
6. J. Álvarez 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: Geotemas (Madrid)

Resumen

We describe and study structural evidences concerning to Alpine tectonics at NE sector of the Spanish Central System (SCS). In Valdesotos area, the Hercynian basement is uplifted over Mesozoic sediments, throughout a main SW verging thrust. Fault population analysis and geological mappinghas been used to look at the relation between structures in the basement and in the cover. As a consequence of accommodation of strains in the basement, kink folds are developed, such as secondary thrust and folds in the tegument. All these meso- and macrostructures seem to answer to ashortening in agreement with the Cenozoic deformation.

Fuente de los datos: Dialnet