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

Joaquim J Sousa,Juan A Armenteros,Ramon F Hanssen,Pedro Alfaro,Andrew J Hooper,Zbigniew Perski,Luisa C Bastos,Manuel Avilés,Jesús Galindo-Zaldívar,Carlos Sanz De Galdeano,Ma Selmira Garrido,Elena Giménez,Antonio M Ruiz,Antonio J Gil

doi:10.1016/j.protcy.2014.10.040

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

Joaquim J Sousa, Juan A Armenteros + Show 12 more

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https://doi.org/10.1016/j.protcy.2014.10.040

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Journal: Procedia Technology	Publication Date: Jan 1, 2014
Citations: 25	License type: cc-by-nc-nd

Affiliation: University of Porto, University of Jaén, Delft University of Technology, University of Alicante, University of Leeds, Polish Geological Institute, University of Granada, Instituto Andaluz de Ciencias de la Tierra, Spanish National Research Council

#Central Betic Cordillera #Active Tectonic Structures + Show 8 more

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Abstract

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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