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

Autor: Sousa, Joaquim J., Ruiz, Antonio M., Hooper, Andrew J., Hanssen, Ramon F., Perski, Zbigniew, Bastos, Luisa C., Gil, Antonio J., Galindo-Zaldívar, Jesús, Galdeano, Carlos Sanz de, Alfaro, Pedro, Garrido, M a Selmira, Armenteros, Juan A., Giménez, Elena, Avilés, Manuel
Zdroj: Procedia Technology; 2014, Vol. 16, p886-896, 11p
Abstrakt: 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. [ABSTRACT FROM AUTHOR]
Databáze: Supplemental Index