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

Authors :
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)
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)
Publication Year :
2014

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.<br />Geoscience & Remote Sensing<br />Civil Engineering and Geosciences

Details

Database :
OAIster
Notes :
English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1008821741
Document Type :
Electronic Resource
Full Text :
https://doi.org/10.1016.j.protcy.2014.10.040