Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry

Antonio M. Ruiz-Armenteros; J. Manuel Delgado; Joaquim J. Sousa; Ramon F. Hanssen; Miguel Caro; Antonio J. Gil; Jesús Galindo-Zaldivar; Carlos Sanz de Galdeano

doi:10.5270/Fringe2015

Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry

Antonio M. Ruiz-Armenteros, J. Manuel Delgado, Joaquim J. Sousa, Ramon F. Hanssen, Miguel Caro, Antonio J. Gil, Jesús Galindo-Zaldivar, Carlos Sanz de Galdeano

Mathematical Geodesy and Positioning

Research output: Chapter in Book/Conference proceedings/Edited volume › Conference contribution › Scientific › peer-review

1 Citation (Scopus)

29 Downloads (Pure)

Abstract

The Betic-Rif cordilleras are build-up in the western Mediterranean by the deformations related to the Eurasian-African plate boundary. The recent NW-SE convergence produces the simultaneous development of large folds and faults in the central part of the Internal Zones of the Betic Cordilleras, which continues active up to Present. The uplift of the mountain ranges is mainly related to the development of folds in this regional compressive setting. Sierra Tejeda constitutes a relief related to the development of a complex shaped recent antiform that is located near the coast line. At the northern limb of Sierra Tejeda is located the Zafarraya fault, a high-angle northwards dipping normal fault. Understanding the tectonic of the Zafarraya fault is crucial since one of the most destructive earthquakes (25th December 1884) on the Iberian Peninsula occurred along this fault (magnitude of 6.7). This paper investigates the applicability of satellite radar interferometry using ERS-1/2 SAR and Envisat ASAR datasets to help to constraint the geological hazard in this part of the
Betic Cordillera.

Original language	English
Title of host publication	Proceedings of the Fringe 2015 Workshop
Subtitle of host publication	Frascati, Italy 23–27 March 2015 (ESA SP-731, May 2015)
Editors	L. Ouwehand
Publisher	ESA Publication
Number of pages	7
Volume	SP-731
ISBN (Print)	9789292212957
DOIs	https://doi.org/10.5270/Fringe2015
Publication status	Published - 2015
Event	Fringe 2015 workshop, Frascati, Italy - Noordwijk Duration: 23 Mar 2015 → 27 Mar 2015

Conference

Conference	Fringe 2015 workshop, Frascati, Italy
Period	23/03/15 → 27/03/15

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10.5270/Fringe2015

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Ruiz-Armenteros, A. M., Delgado, J. M., Sousa, J. J., Hanssen, R. F., Caro, M., Gil, A. J., Galindo-Zaldivar, J., & Sanz de Galdeano, C. (2015). Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry. In L. Ouwehand (Ed.), Proceedings of the Fringe 2015 Workshop: Frascati, Italy 23–27 March 2015 (ESA SP-731, May 2015) (Vol. SP-731). Article 75 ESA Publication. https://doi.org/10.5270/Fringe2015

@inproceedings{532500cc423244119f2d9606a017df09,

title = "Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry",

abstract = "The Betic-Rif cordilleras are build-up in the western Mediterranean by the deformations related to the Eurasian-African plate boundary. The recent NW-SE convergence produces the simultaneous development of large folds and faults in the central part of the Internal Zones of the Betic Cordilleras, which continues active up to Present. The uplift of the mountain ranges is mainly related to the development of folds in this regional compressive setting. Sierra Tejeda constitutes a relief related to the development of a complex shaped recent antiform that is located near the coast line. At the northern limb of Sierra Tejeda is located the Zafarraya fault, a high-angle northwards dipping normal fault. Understanding the tectonic of the Zafarraya fault is crucial since one of the most destructive earthquakes (25th December 1884) on the Iberian Peninsula occurred along this fault (magnitude of 6.7). This paper investigates the applicability of satellite radar interferometry using ERS-1/2 SAR and Envisat ASAR datasets to help to constraint the geological hazard in this part of theBetic Cordillera.",

author = "Ruiz-Armenteros, {Antonio M.} and Delgado, {J. Manuel} and Sousa, {Joaquim J.} and Hanssen, {Ramon F.} and Miguel Caro and Gil, {Antonio J.} and Jes{\'u}s Galindo-Zaldivar and {Sanz de Galdeano}, Carlos",

year = "2015",

doi = "10.5270/Fringe2015",

language = "English",

isbn = "9789292212957",

volume = "SP-731",

editor = "L. Ouwehand",

booktitle = "Proceedings of the Fringe 2015 Workshop",

publisher = "ESA Publication",

note = "Fringe 2015 workshop, Frascati, Italy ; Conference date: 23-03-2015 Through 27-03-2015",

}

Ruiz-Armenteros, AM, Delgado, JM, Sousa, JJ, Hanssen, RF, Caro, M, Gil, AJ, Galindo-Zaldivar, J & Sanz de Galdeano, C 2015, Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry. in L Ouwehand (ed.), Proceedings of the Fringe 2015 Workshop: Frascati, Italy 23–27 March 2015 (ESA SP-731, May 2015) . vol. SP-731, 75, ESA Publication, Fringe 2015 workshop, Frascati, Italy, 23/03/15. https://doi.org/10.5270/Fringe2015

Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry. / Ruiz-Armenteros, Antonio M.; Delgado, J. Manuel; Sousa, Joaquim J. et al.
Proceedings of the Fringe 2015 Workshop: Frascati, Italy 23–27 March 2015 (ESA SP-731, May 2015) . ed. / L. Ouwehand. Vol. SP-731 ESA Publication, 2015. 75.

Research output: Chapter in Book/Conference proceedings/Edited volume › Conference contribution › Scientific › peer-review

TY - GEN

T1 - Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry

AU - Ruiz-Armenteros, Antonio M.

AU - Delgado, J. Manuel

AU - Sousa, Joaquim J.

AU - Hanssen, Ramon F.

AU - Caro, Miguel

AU - Gil, Antonio J.

AU - Galindo-Zaldivar, Jesús

AU - Sanz de Galdeano, Carlos

PY - 2015

Y1 - 2015

N2 - The Betic-Rif cordilleras are build-up in the western Mediterranean by the deformations related to the Eurasian-African plate boundary. The recent NW-SE convergence produces the simultaneous development of large folds and faults in the central part of the Internal Zones of the Betic Cordilleras, which continues active up to Present. The uplift of the mountain ranges is mainly related to the development of folds in this regional compressive setting. Sierra Tejeda constitutes a relief related to the development of a complex shaped recent antiform that is located near the coast line. At the northern limb of Sierra Tejeda is located the Zafarraya fault, a high-angle northwards dipping normal fault. Understanding the tectonic of the Zafarraya fault is crucial since one of the most destructive earthquakes (25th December 1884) on the Iberian Peninsula occurred along this fault (magnitude of 6.7). This paper investigates the applicability of satellite radar interferometry using ERS-1/2 SAR and Envisat ASAR datasets to help to constraint the geological hazard in this part of theBetic Cordillera.

AB - The Betic-Rif cordilleras are build-up in the western Mediterranean by the deformations related to the Eurasian-African plate boundary. The recent NW-SE convergence produces the simultaneous development of large folds and faults in the central part of the Internal Zones of the Betic Cordilleras, which continues active up to Present. The uplift of the mountain ranges is mainly related to the development of folds in this regional compressive setting. Sierra Tejeda constitutes a relief related to the development of a complex shaped recent antiform that is located near the coast line. At the northern limb of Sierra Tejeda is located the Zafarraya fault, a high-angle northwards dipping normal fault. Understanding the tectonic of the Zafarraya fault is crucial since one of the most destructive earthquakes (25th December 1884) on the Iberian Peninsula occurred along this fault (magnitude of 6.7). This paper investigates the applicability of satellite radar interferometry using ERS-1/2 SAR and Envisat ASAR datasets to help to constraint the geological hazard in this part of theBetic Cordillera.

UR - http://seom.esa.int/fringe2015/page_session28.php#75p

U2 - 10.5270/Fringe2015

DO - 10.5270/Fringe2015

M3 - Conference contribution

SN - 9789292212957

VL - SP-731

BT - Proceedings of the Fringe 2015 Workshop

A2 - Ouwehand, L.

PB - ESA Publication

T2 - Fringe 2015 workshop, Frascati, Italy

Y2 - 23 March 2015 through 27 March 2015

ER -

Ruiz-Armenteros AM, Delgado JM, Sousa JJ, Hanssen RF, Caro M, Gil AJ et al. Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry. In Ouwehand L, editor, Proceedings of the Fringe 2015 Workshop: Frascati, Italy 23–27 March 2015 (ESA SP-731, May 2015) . Vol. SP-731. ESA Publication. 2015. 75 doi: 10.5270/Fringe2015

Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry

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