Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10186
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dc.contributor.authorallCianflone, G.; Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15B, 87036 Arcavacata di Rende (Cs), Italyen
dc.contributor.authorallTolomei, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallBrunori, C. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallDominici, R.; Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15B, 87036 Arcavacata di Rende (Cs), Italyen
dc.date.accessioned2015-11-30T12:03:19Zen
dc.date.available2015-11-30T12:03:19Zen
dc.date.issued2015-11-30en
dc.identifier.urihttp://hdl.handle.net/2122/10186en
dc.description.abstractWe applied the Small Baseline Subset multi-temporal InSAR technique (SBAS) to two SAR datasets acquired from 2003 up to 2013 by Envisat (ESA, European Space Agency) and COSMO-SkyMed (ASI, Italian Space Agency) satellites to investigate spatial and temporal patterns of land subsidence in the Sibari Plain (Southern Italy). Subsidence processes (up to ~20 mm/yr) were investigated comparing geological, hydrogeological, and land use information with interferometric results. We suppose a correlation between subsidence and thickness of the Plio-Quaternary succession suggesting an active role of the isostatic compensation. Furthermore, the active back thrusting in the Corigliano Gulf could trigger a flexural subsidence mechanism even if fault activity and earthquakes do not seem play a role in the present subsidence. In this context, the compaction of Holocene deposits contributes to ground deformation. Despite the rapid urbanization of the area in the last 50 years, we do not consider the intensive groundwater pumping and related water table drop as the main triggering cause of subsidence phenomena, in disagreement with some previous publications. Our interpretation for the deformation fields related to natural and anthropogenic factors would be a comprehensive and exhaustive justification to the complexity of subsidence processes in the Sibari Plain.en
dc.description.sponsorshipPON (Operational National Plan) 2007–2013 from MIUR (Italian Research Ministry of Research) Project AMICUS (Study for the environmental protection and the mitigation of Anthropogenic Pollution In the Coastal Environment of selected areas of Calabria; ID: PON01_ 02818) - COSMO-SkyMed® PRODUCTS, © ASI (Italian Space Agency)—provided under license of ASI in the framework of the S3 Project “Short term earthquake prediction and preparation” (DPC-INGV, 2013). The Envisat images are provided by ESA (European Space Agency) under the CAT.1P 5605en
dc.language.isoEnglishen
dc.publisher.nameMolecular Diversity Preservation Internationalen
dc.relation.ispartofRemote Sensingen
dc.relation.ispartofseries7(2015)en
dc.relation.isversionofhttp://www.mdpi.com/2072-4292/7/12/15812/htmlen
dc.subjectSBAS-InSARen
dc.subjectSibari Plainen
dc.subjectsubsidenceen
dc.subjectgeologyen
dc.subjectanthropic processesen
dc.titleInSAR Time Series Analysis of Natural and Anthropogenic Coastal Plain Subsidence: The Case of Sibari (Southern Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber16004–16023en
dc.identifier.URLhttp://www.mdpi.com/2072-4292/7/12/15812/htmlen
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesyen
dc.identifier.doi10.3390/rs71215812en
dc.description.obiettivoSpecifico6A. Monitoraggio ambientale, sicurezza e territorioen
dc.description.obiettivoSpecifico1IT. Reti di monitoraggio e Osservazionien
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn2072-4292en
dc.contributor.authorCianflone, G.en
dc.contributor.authorTolomei, C.en
dc.contributor.authorBrunori, C. A.en
dc.contributor.authorDominici, R.en
dc.contributor.departmentDepartment of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15B, 87036 Arcavacata di Rende (Cs), Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentDepartment of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15B, 87036 Arcavacata di Rende (Cs), Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità della Calabria-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.deptDepartment of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15B, 87036 Arcavacata di Rende (Cs), Italy-
crisitem.author.orcid0000-0002-2729-9415-
crisitem.author.orcid0000-0001-7378-0712-
crisitem.author.orcid0000-0003-0862-8161-
crisitem.author.orcid0000-0003-4223-1512-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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