Cuantificación del desplazamiento dextroso Alpino en la cordillera Ibérica a partir de datos gravimétricos.

  1. Bergamín, J.F. 1
  2. De Vicente, G. 1
  3. Tejero, R. 1
  4. Sánchez Serrano, F. 1
  5. Gómez, D. 1
  6. Muñoz Martín, A. 1
  7. Perucha, M. A. 1
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1996

Título del ejemplar: Comunicaciones presentadas en el IV Congreso Nacional de Geología, Alcalá de Henares, 1996

Número: 20

Páginas: 917-920

Tipo: Artículo

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Otras publicaciones en: Geogaceta

Resumen

lntraplate deformation in the eastern zone of the iberian Peninsula is characterized by strike-slip faulting during Tertiary. Gradient pattern of Bouguer Anomaly Map of the Spanish Central System-Iberian Range linking zone are related to main crustal faults. Gradients pattern has been analysed by means of a raster type Geographic lnformation System. Two main gradien orientations associated with Spanish Central System structures (NE-SW) and with iberian Range structures (NW-SE) have been established. Gradient map and artificial shading image have been used to quantify dextral slip along NOSE faults. Slip value reach a figure of 34 km. Assuming that the slip began in Oligocene times, movement rate between the Spanish Central System and the lberian Range Castilian Branch is 0.93 mm/y. Considering a Middle Miocene start a 2.2 mm/y slip rate is computed.

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