Cortes compensados para la deformación principal alpina en el borde sur oriental del Sistema Central español (Zona de Tamajón, Guadalajara)

  1. F. Sánchez Serrano 1
  2. G. de Vicente Muñoz 1
  3. J. M. González Casado 2
  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:
Revista de la Sociedad Geológica de España

ISSN: 0214-2708

Datum der Publikation: 1993

Ausgabe: 6

Nummer: 1-2

Seiten: 7-14

Art: Artikel

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Andere Publikationen in: Revista de la Sociedad Geológica de España

Zusammenfassung

The main Alpine structures in the SE border of the Spanish Central System (Tamajón zone), have been found to be two thrust faults with N70°E trend, and transport direction towards SE, associated with secondary backthrusts and transfer faults. The tectonic transport direction fits well the shortening direction of the "Guadarrama" stage of compression (N150°E). The effects of thrusting in the Mesozoic cover is the development of assimetric folds. The ammount of shortening in this zone, deduced from cross-section balancing, is about 17-19%.

Fuente de los datos: Dialnet