Multi-temporal InSAR for Deformation Monitoring of the Granada and Padul Faults and the Surrounding Area (Betic Cordillera, Southern Spain)

  1. Sousa, Joaquim J.
  2. Ruiz, Antonio M.
  3. Hooper, Andrew J.
  4. Hanssen, Ramon F.
  5. Perski, Zbigniew
  6. Bastos, Luisa C.
  7. Gil, Antonio J.
  8. Galindo-Zaldívar, Jesús
  9. Galdeano, Carlos Sanz de
  10. Alfaro, Pedro
  11. Garrido, Ma Selmira
  12. Armenteros, Juan A.
  13. Giménez, Elena
  14. Avilés, Manuel
Revista:
Procedia Technology

ISSN: 2212-0173

Año de publicación: 2014

Volumen: 16

Páginas: 886-896

Tipo: Artículo

DOI: 10.1016/J.PROTCY.2014.10.040 GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Procedia Technology

Resumen

The quantification of low rate active tectonic structures is a major target of geodetic and geological studies to improve the knowledge of seismic hazards. The central Betic Cordillera (southern Spain) is affected by moderately active tectonic structures and seismicity. Part of this seismic activity is produced by several NW-SE normal faults located in the E of the Granada Basin.

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