Crustal velocity and strain rate fields in the Balearic Islands based on continuous GPS time series from the XGAIB network (2010-2013)

Please use this identifier to cite or link to this item: http://hdl.handle.net/10045/37962
Full metadata record
Full metadata record
DC FieldValueLanguage
dc.contributorEvolución Geodinámica de la Cordillera Bética Oriental y de la Plataforma Marina de Alicantees
dc.contributor.authorSánchez Alzola, Alberto-
dc.contributor.authorSánchez, Carlos-
dc.contributor.authorGiménez, Jordi-
dc.contributor.authorAlfaro García, Pedro-
dc.contributor.authorGelabert, Bernadí-
dc.contributor.authorBorque Arancón, María Jesús-
dc.contributor.authorGil Cruz, Antonio José-
dc.contributor.otherUniversidad de Alicante. Departamento de Ciencias de la Tierra y del Medio Ambientees
dc.date.accessioned2014-06-11T10:27:44Z-
dc.date.available2014-06-11T10:27:44Z-
dc.date.issued2014-06-04-
dc.identifier.citationJournal of Geodynamics. 2014, Accepted Manuscript. doi:10.1016/j.jog.2014.05.005es
dc.identifier.issn0264-3707 (Print)-
dc.identifier.issn1879-1670 (Online)-
dc.identifier.urihttp://hdl.handle.net/10045/37962-
dc.description.abstractIn this paper, we present a first estimation, using the GIPSY-OASIS software, of the crustal velocity and strain rate fields in the Balearic Islands (Spain), based on continuous GPS observations from the XGAIB network spanning the period 2010-2013. The XGAIB network consists of nine permanent, widely distributed stations that have operated continuously since 2010. In this paper, we describe the XGAIB network and the CGPS data processing and present our principle results in terms of the position time series and velocities of all of the sites, which were observed for more than three and a half years. In addition, strain tensors were estimated from the velocity field to obtain the first realistic crustal deformation model of the archipelago. The strains exhibit gradual variation across the Balearic Islands, from WNW-ESE extension in the southwest (Ibiza and Formentera) to NW-SE compression in the northeast (Menorca). These results constitute an advance in our knowledge of the tectonics of the western Mediterranean region.es
dc.description.sponsorshipThis research was partly funded by the Spanish Ministry of Science and Innovation through the AYA2010-15501, CGL2011-30153-C02-02 and CSD2006-0041 projects (European Regional Development Fund-ERDF).es
dc.languageenges
dc.publisherElsevieres
dc.subjectCGPSes
dc.subjectPrecise point positioninges
dc.subjectCrustal deformationes
dc.subjectTime serieses
dc.subjectBalearic Islandses
dc.subject.otherGeodinámica Internaes
dc.titleCrustal velocity and strain rate fields in the Balearic Islands based on continuous GPS time series from the XGAIB network (2010-2013)es
dc.typeinfo:eu-repo/semantics/articlees
dc.peerreviewedsies
dc.identifier.doi10.1016/j.jog.2014.05.005-
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.jog.2014.05.005es
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
Appears in Collections:INV - GEODIN - Artículos de Revistas

Files in This Item:
Files in This Item:
File Description SizeFormat 
Thumbnail2014_Sanchez-Alzola_etal_JG.pdfAccepted Manuscript (acceso abierto)999,34 kBAdobe PDFOpen Preview


Items in RUA are protected by copyright, with all rights reserved, unless otherwise indicated.