Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)

The Campo de Dalias is an area with relevant seismicity associated to the active tectonic deformations of the southern boundary of the Betic Cordillera. A non-permanent GPS network was installed to monitor, for the first time, the fault- and fold-related activity. In addition, two high precision lev...

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Main Authors: Carlos Marín-Lechado, Jesús Galindo-Zaldívar, Antonio José Gil, María Jesús Borque, María Clara de Lacy, Antonio Pedrera, Angel Carlos López-Garrido, Pedro Alfaro, Francisco García-Tortosa, Maria Isabel Ramos, Gracia Rodríguez-Caderot, José Rodríguez-Fernández, Ana Ruiz-Constán, Carlos Sanz de Galdeano-Equiza
Format: Article
Language:English
Published: MDPI AG 2010-04-01
Series:Sensors
Subjects:
GPS
Online Access:http://www.mdpi.com/1424-8220/10/4/3504/
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spelling doaj-3365d5d5744b48ee916afa37607793612020-11-25T01:26:55ZengMDPI AGSensors1424-82202010-04-011043504351810.3390/s100403504Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)Carlos Marín-LechadoJesús Galindo-ZaldívarAntonio José GilMaría Jesús BorqueMaría Clara de LacyAntonio PedreraAngel Carlos López-GarridoPedro AlfaroFrancisco García-TortosaMaria Isabel RamosGracia Rodríguez-CaderotJosé Rodríguez-FernándezAna Ruiz-ConstánCarlos Sanz de Galdeano-EquizaThe Campo de Dalias is an area with relevant seismicity associated to the active tectonic deformations of the southern boundary of the Betic Cordillera. A non-permanent GPS network was installed to monitor, for the first time, the fault- and fold-related activity. In addition, two high precision levelling profiles were measured twice over a one-year period across the Balanegra Fault, one of the most active faults recognized in the area. The absence of significant movement of the main fault surface suggests seismogenic behaviour. The possible recurrence interval may be between 100 and 300 y. The repetitive GPS and high precision levelling monitoring of the fault surface during a long time period may help us to determine future fault behaviour with regard to the existence (or not) of a creep component, the accumulation of elastic deformation before faulting, and implications of the fold-fault relationship. http://www.mdpi.com/1424-8220/10/4/3504/seismogenic faultslarge foldsactive tectonicsprecise levellingGPSwestern Mediterranean
collection DOAJ
language English
format Article
sources DOAJ
author Carlos Marín-Lechado
Jesús Galindo-Zaldívar
Antonio José Gil
María Jesús Borque
María Clara de Lacy
Antonio Pedrera
Angel Carlos López-Garrido
Pedro Alfaro
Francisco García-Tortosa
Maria Isabel Ramos
Gracia Rodríguez-Caderot
José Rodríguez-Fernández
Ana Ruiz-Constán
Carlos Sanz de Galdeano-Equiza
spellingShingle Carlos Marín-Lechado
Jesús Galindo-Zaldívar
Antonio José Gil
María Jesús Borque
María Clara de Lacy
Antonio Pedrera
Angel Carlos López-Garrido
Pedro Alfaro
Francisco García-Tortosa
Maria Isabel Ramos
Gracia Rodríguez-Caderot
José Rodríguez-Fernández
Ana Ruiz-Constán
Carlos Sanz de Galdeano-Equiza
Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)
Sensors
seismogenic faults
large folds
active tectonics
precise levelling
GPS
western Mediterranean
author_facet Carlos Marín-Lechado
Jesús Galindo-Zaldívar
Antonio José Gil
María Jesús Borque
María Clara de Lacy
Antonio Pedrera
Angel Carlos López-Garrido
Pedro Alfaro
Francisco García-Tortosa
Maria Isabel Ramos
Gracia Rodríguez-Caderot
José Rodríguez-Fernández
Ana Ruiz-Constán
Carlos Sanz de Galdeano-Equiza
author_sort Carlos Marín-Lechado
title Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)
title_short Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)
title_full Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)
title_fullStr Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)
title_full_unstemmed Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain)
title_sort levelling profiles and a gps network to monitor the active folding and faulting deformation in the campo de dalias (betic cordillera, southeastern spain)
publisher MDPI AG
series Sensors
issn 1424-8220
publishDate 2010-04-01
description The Campo de Dalias is an area with relevant seismicity associated to the active tectonic deformations of the southern boundary of the Betic Cordillera. A non-permanent GPS network was installed to monitor, for the first time, the fault- and fold-related activity. In addition, two high precision levelling profiles were measured twice over a one-year period across the Balanegra Fault, one of the most active faults recognized in the area. The absence of significant movement of the main fault surface suggests seismogenic behaviour. The possible recurrence interval may be between 100 and 300 y. The repetitive GPS and high precision levelling monitoring of the fault surface during a long time period may help us to determine future fault behaviour with regard to the existence (or not) of a creep component, the accumulation of elastic deformation before faulting, and implications of the fold-fault relationship.
topic seismogenic faults
large folds
active tectonics
precise levelling
GPS
western Mediterranean
url http://www.mdpi.com/1424-8220/10/4/3504/
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