Distribución de facies y evolución de la sedimentación aluvial cuaternaria en el extremo suroccidental de Sierra Nevada (Cordillera Bética)

  1. C. Viseras 1
  2. J. Fernández 1
  3. J.M. Soria 2
  4. F. García 3
  1. 1 Universidad de Granada
    info

    Universidad de Granada

    Granada, España

    ROR https://ror.org/04njjy449

  2. 2 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

  3. 3 Universidad de Jaén
    info

    Universidad de Jaén

    Jaén, España

    ROR https://ror.org/0122p5f64

Erakutsi afiliazioak +
Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2004

Zenbakien izenburua: IV Congreso Geológico de España

Zenbakia: 6

Orrialdeak: 139-142

Mota: Artikulua

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Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

Ten minor architectural elements have been identified in the Quaternary alluvial fans lying against the Padul Fault (SW border of Sierra Nevada, Betic Cordillera) that combine to build up two types of major architectural elements that correspond to: (!) former positions of the incised channels and (2) accretionary lobes developed below the intersection point. The fan apex, the proximal, medial and distal fan areas are characterised by particular proportions of the ten minor architectural elements.

Datuen iturria: Dialnet