Marco tectónico de la unidad hidrogeológica del Campo de Montiel (provincias de Ciudad Real y Albacete, España central)

  1. P.J. Rincón 1
  2. E. Montero 1
  3. R. Vega 1
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

Journal:
Revista de la Sociedad Geológica de España

ISSN: 0214-2708

Year of publication: 2001

Volume: 14

Issue: 3-4

Pages: 213-226

Type: Article

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Abstract

The direction of runoff and underground flow in the Campo de Montiel aquifer (Central Spain), its internal thresholds, the location of springs, the flowing of rivers into three different catchment basins (Guadiana, Guadalquivir and Júcar) as well as the origin of the Lagunas de Ruidera Parkland are the result of a ductile and brittle deformation. The spatial distribution of crustal flexures, folds, joints and ENE-WSW, NW-SE and NNE-SSW faults and fracture zones are due to a weak intraplate compressive stress field transmitted from the Betic border (< 9 Ma).

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