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
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  2. 2 Universidad Autónoma de Madrid
    info

    Universidad Autónoma de Madrid

    Madrid, España

    ROR https://ror.org/01cby8j38

Zeitschrift:
Geotemas (Madrid)

ISSN: 1576-5172

Datum der Publikation: 2004

Titel der Ausgabe: VI CONGRESO GEOLÓGICO DE ESPAÑA, ZARAGOZA, 12-15 JULIO, 2004

Nummer: 6

Seiten: 237-240

Art: Artikel

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Andere Publikationen in: Geotemas (Madrid)

Zusammenfassung

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