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Establishment of a non-permanent GPS network to monitor deformations in Zafarraya Fault and Sierra Tejeda Antiform (Spain)

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dc.creator Borque Arancón, María Jesús
dc.creator Galindo-Zaldívar, Jesús
dc.creator Gil, Alejandro J.
dc.creator Jabaloy, Antonio
dc.creator Lacy Pérez de los Cobos, M.ª Clara de
dc.creator López-Garrido, A. C.
dc.creator Rodríguez Caderot, Gracia
dc.creator Ruíz Armenteros, Antonio
dc.creator Sanz de Galdeano, Carlos
dc.date 2008-05-23T10:25:55Z
dc.date 2008-05-23T10:25:55Z
dc.date 2005
dc.date.accessioned 2017-01-31T01:26:57Z
dc.date.available 2017-01-31T01:26:57Z
dc.identifier Física de la Tierra 2005, 17, 23-31
dc.identifier 0214-4557 (Print)
dc.identifier 1988-2440 (Online)
dc.identifier http://hdl.handle.net/10261/4491
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/4491
dc.description The NW-SE to NNW-SSE convergence between the African and Eurasian plates in the western Mediterranean has developed the recent relief of the Betic-Rif Cordilleras. The central part of the Internal Zones of the Betic Cordilleras is deformed by large open folds and faults, mainly with normal character. The Zafarraya fault, located to the N of the Sierra Tejeda antiform, was active during the 1884 Andalusia earthquake of 6.7 estimated magnitude. In the framework of an interdisciplinary research project, a non-permanent GPS-network has been established at Zafarraya Fault and Sierra Tejeda antiform to monitor deformations related to these active tectonic structures.
dc.description Peer reviewed
dc.format 3798409 bytes
dc.format application/pdf
dc.language eng
dc.publisher Universidad Complutense de Madrid
dc.rights openAccess
dc.subject Active Tectonics
dc.subject GPS Network
dc.subject Zafarraya Fault
dc.subject Sierra Tejeda Antiform
dc.subject Betic Cordillera
dc.title Establishment of a non-permanent GPS network to monitor deformations in Zafarraya Fault and Sierra Tejeda Antiform (Spain)
dc.type Artículo


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