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dc.contributor.authorCorominas Dulcet, Jordi
dc.contributor.authorIglesias González, Rubén
dc.contributor.authorAguasca Solé, Alberto
dc.contributor.authorMallorquí Franquet, Jordi Joan
dc.contributor.authorFabregas Canovas, Francisco Javier
dc.contributor.authorPlanas, Xavier
dc.contributor.authorGili Ripoll, José Antonio
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria del Terreny, Cartogràfica i Geofísica
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Teoria del Senyal i Comunicacions
dc.date.accessioned2014-10-01T18:27:08Z
dc.date.created2014
dc.date.issued2014
dc.identifier.citationCorominas, J. [et al.]. Comparing satellite based and ground based radar interferometry and field observations at the Canillo landslide (Pyrenees). A: International IAEG Congress. "Engineering Geology for Society and Territory: volume 2: Landslide Processes". Torino: Springer, 2014, p. 333-338.
dc.identifier.isbn978-3-319-09056-6
dc.identifier.urihttp://hdl.handle.net/2117/24201
dc.description.abstractThe landslide of El Forn de Canillo in the Principality of Andorra is one of the largest in the Pyrenees. In 2007 a monitoring system (boreholes equipped with inclinometers, extensometers and piezometers) was set up. Between 2010 and 2011, surface displacements were measured using differential interferometry techniques (GB-SAR and DInSAR). The interferograms of both radars have yielded mutually consistent results, compatible with the inclinometric measures. Furthermore, the observations with TerraSAR-X, with greater spatial coverage, have shown that the displacements are significantly higher in the upper part of the slope (up to 4 cm/year). Field surveys evidenced the presence of activity indicators (open tension cracks, ground disturbance and structural damages) that confirm the existence of these movements. In El Forn landslide, the combined use of radar techniques with conventional instrumentation allows for a more complete and representative interpretation of the behavior of the slope.
dc.format.extent6 p.
dc.language.isoeng
dc.publisherSpringer
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Riscos geològics
dc.subject.lcshLandslides--Monitoring
dc.subject.lcshAndorra
dc.subject.otherMonitoring
dc.subject.otherDinsar
dc.subject.otherGB-SAR
dc.titleComparing satellite based and ground based radar interferometry and field observations at the Canillo landslide (Pyrenees)
dc.typeConference report
dc.subject.lemacEsllavissades -- Pirineus
dc.contributor.groupUniversitat Politècnica de Catalunya. RSLAB - Grup de Recerca en Teledetecció
dc.contributor.groupUniversitat Politècnica de Catalunya. EGEO - Enginyeria Geomàtica
dc.contributor.groupUniversitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques
dc.identifier.doi10.1007/978-3-319-09057-3
dc.rights.accessRestricted access - publisher's policy
drac.iddocument15182681
dc.description.versionPostprint (published version)
dc.date.lift10000-01-01
upcommons.citation.authorCorominas, J.; Iglesias, R.; Aguasca, A.; Mallorqui, J.J.; Fabregas, F.; Planas, X.; Gili, J.
upcommons.citation.contributorInternational IAEG Congress
upcommons.citation.pubplaceTorino
upcommons.citation.publishedtrue
upcommons.citation.publicationNameEngineering Geology for Society and Territory: volume 2: Landslide Processes
upcommons.citation.startingPage333
upcommons.citation.endingPage338


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