Pure and Applied Geophysics

, Volume 164, Issue 1, pp 1–21

Mountain Front Development by Folding and Crustal Thickening in the Internal Zone of the Betic Cordillera-Alboran Sea Boundary


    • Instituto Geológico y Minero de España
  • Jesús Galindo-Zaldívar
    • Departamento de GeodinámicaUniversidad de Granada
  • Luís Roberto Rodríguez-Fernández
    • Instituto Geológico y Minero de España
  • Antonio Pedrera
    • Departamento de GeodinámicaUniversidad de Granada

DOI: 10.1007/s00024-006-0157-4

Cite this article as:
Marín-Lechado, C., Galindo-Zaldívar, J., Rodríguez-Fernández, L.R. et al. Pure appl. geophys. (2007) 164: 1. doi:10.1007/s00024-006-0157-4


The boundary between the Alboran Sea and Betic Cordillera is a good example of a fold related mountain front in the Internal Zone of an alpine mountain range. Since the late Miocene, NNW-SSE convergence between the Eurasian and African plates has produced shortening and related orthogonal extension. To improve the characterisation of the geometry of the deep structure in the region and to establish the recent tectonic evolution of the mountain front, well logs and newly acquired geophysical data (multichannel reflection seismic and gravimetric surveys) have been interpreted and integrated with available surface data. The most marked tectonic structure corresponds to large antiforms and synforms of ENE-WSW trend which are related to mountain ranges and basins, respectively. The fold belt continues toward the northern continental shelf of the Alboran Sea. The fold vergence is generally northwards and its amplitude decreases progressively towards SSE, until disappearring in a sharp boundary where the reflectors are undeformed. The deep geometry suggests that fold growth started during upper Tortonian times and continued its activity up to Pliocene or even Quaternary times. The NNW-SSE compression produces crustal thickening and a regional and progressive southwards emersion. The location of main present-day deformation fronts in the Internal Zones contrasts with classical models where the deformation progresses towards the frontal part of External Zones of cordilleras. In addition, this fold-related deformation mountain front has features different from fault related fronts, as it does not show a sharp boundary, and folds that determine rectilinear mountain boundaries decrease progressively in amplitude or in wavelength up to undeformed areas.


Active foldsNeogene-Quaternary basincontinental upliftgeophysical prospectingwestern Mediterranean
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© Birkhäuser Verlag, Basel, 2007