Intervalos de recurrencia de la zona de falla de Baza para el intervalo Pleistoceno superior-Holoceno

  1. I. Martin-Rojas 1
  2. J. Castro 1
  3. I. Medina 1
  4. F.J. García-Tortosa 2
  5. P. Alfaro 1
  1. 1 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

  2. 2 Universidad de Jaén
    info

    Universidad de Jaén

    Jaén, España

    ROR https://ror.org/0122p5f64

Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2016

Zenbakien izenburua: IX CONGRESO GEOLÓGICO DE ESPAÑA

Zenbakia: 16

Orrialdeak: 523-526

Mota: Artikulua

DIALNET GOOGLE SCHOLAR lock_openSarbide irekia editor

Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

We here presentthe first paleoseismic data of the Baza Fault Zone (central Betic Cordillera, Spain). We carried out a geomorpholic and stratigrpahic analysis of the units located near to the fault. After that, we selected three sites where we excavated up to five paleoseismic trenches. We discuss trenches logs in terms of paleoseismic events. These data together with numeric dates permit us to estimate a recurrence interval of 5661-8990 years for surface rupturing events occurred in the Baza Fault Zone for the last 42 ky.

Datuen iturria: Dialnet