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

Any de publicació: 2014

Volum: 16

Pàgines: 886-896

Tipus: Article

DOI: 10.1016/J.PROTCY.2014.10.040 GOOGLE SCHOLAR lock_openAccés obert editor

Altres publicacions en: Procedia Technology

Resum

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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