Segmentación y evolución reciente del Sistema de Fallas de la Sierra de Carrascoyimplicaciones en su potencial sismogénico

  1. Martín Banda, Raquel
Supervised by:
  1. Julián García Mayordomo Director
  2. Juan M. Insua Arévalo Director

Defence university: Universidad Complutense de Madrid

Fecha de defensa: 02 October 2020

Committee:
  1. José Jesús Martínez Díaz Chair
  2. Héctor Perea Manera Secretary
  3. Carolina Canora Catalán Committee member
  4. María Ortuño Candela Committee member
  5. Eulàlia Masana Closa Committee member
Department:
  1. Geodinámica, Estratigrafía y Paleontología

Type: Thesis

Teseo: 155396 DIALNET lock_openDocta Complutense editor

Abstract

The convergence between the Nubian and Eurasian plates in the western Mediterranean (4,5 - 5,6 mm/a) is mainly absorbed by Tell deformation belt in Algeria northern and by the Eastern Betics Shear Zone (EBSZ), a set of NE-SW actives faults with low slip rates and long seismic loading cycles...