Multi-temporal InSAR for Deformation Monitoring of the Granada and Padul Faults and the Surrounding Area (Betic Cordillera, Southern Spain)
- Sousa, J.J. (author)
- Ruiz, A.M. (author)
- Hooper, A.J. (author)
- Hanssen, R.F. (author)
- Perski, Z. (author)
- Bastos, L.C. (author)
- Gil, A.J. (author)
- Galindo-Zaldivar, J. (author)
- Sanz de Galdeano, C. (author)
- Alfaro, P. (author)
- Garrido, M.S. (author)
- Armenteros, J.A. (author)
- Gimenez, E. (author)
- Aviles, M. (author)
DOIAbstract
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.Geoscience & Remote SensingCivil Engineering and Geoscience
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