{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,9,21]],"date-time":"2026-09-21T04:38:27Z","timestamp":1789965507566,"version":"4.0.1"},"reference-count":70,"publisher":"MDPI AG","issue":"3","license":[{"start":{"date-parts":[[2019,1,28]],"date-time":"2019-01-28T00:00:00Z","timestamp":1548633600000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100003447","name":"State Scholarships Foundation","doi-asserted-by":"publisher","award":["2016-050-0503-8856"],"award-info":[{"award-number":["2016-050-0503-8856"]}],"id":[{"id":"10.13039\/501100003447","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Volcanic history of Santorini over recent years records a seismo-volcanic unrest in 2011\u201312 with a non-eruptive behavior. The volcano deformation state following the unrest was investigated through multi-sensor Synthetic Aperture Radar Interferometry (InSAR) time series. We focused on the analysis of Copernicus Sentinel-1, Radarsat-2 and TerraSAR-X Multi-temporal SAR Interferometric (MT-InSAR) results, for the post-unrest period 2012\u201317. Data from multiple Sentinel-1 tracks and acquisition geometries were used to constrain the E-W and vertical components of the deformation field along with their evolution in time. The interpretation of the InSAR observations and modelling provided insights on the post-unrest deformation pattern of the volcano, allowing the further re-evaluation of the unrest event. The increase of subsidence rates on Nea Kameni, in accordance with the observed change of the spatial deformation pattern, compared to the pre-unrest period, suggests the superimposition of various deformation sources. Best-fitting inversion results indicate two deflation sources located at southwestern Nea Kameni at 1 km depth, and in the northern intra-caldera area at 2 km depth. A northern sill-like source interprets the post-unrest deflation attributed to the passive degassing of the magma intruded at 4 km during the unrest, while an isotropic source at Nea Kameni simulates a prevailing subsidence occurring since the pre-unrest period (1992\u20132010).<\/jats:p>","DOI":"10.3390\/rs11030259","type":"journal-article","created":{"date-parts":[[2019,1,29]],"date-time":"2019-01-29T03:40:55Z","timestamp":1548733255000},"page":"259","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":29,"title":["Multi-Sensor SAR Geodetic Imaging and Modelling of Santorini Volcano Post-Unrest Response"],"prefix":"10.3390","volume":"11","author":[{"given":"Elena","family":"Papageorgiou","sequence":"first","affiliation":[{"name":"School of Geology, Aristotle University of Thessaloniki (AUTh), 54124 Thessaloniki, Greece"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Michael","family":"Foumelis","sequence":"additional","affiliation":[{"name":"BRGM\u2014French Geological Survey, 3 Claude-Guillemin, 45060 Orl\u00e9ans, France"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-2983-045X","authenticated-orcid":false,"given":"Elisa","family":"Trasatti","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia (INGV), 605 Via di Vigna Murata, 00143 Roma, Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9388-9985","authenticated-orcid":false,"given":"Guido","family":"Ventura","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia (INGV), 605 Via di Vigna Murata, 00143 Roma, Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-1715-3743","authenticated-orcid":false,"given":"Daniel","family":"Raucoules","sequence":"additional","affiliation":[{"name":"BRGM\u2014French Geological Survey, 3 Claude-Guillemin, 45060 Orl\u00e9ans, France"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-1813-4878","authenticated-orcid":false,"given":"Antonios","family":"Mouratidis","sequence":"additional","affiliation":[{"name":"School of Geology, Aristotle University of Thessaloniki (AUTh), 54124 Thessaloniki, Greece"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"1968","published-online":{"date-parts":[[2019,1,28]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"39","DOI":"10.1007\/BF02596790","article-title":"L\u2019 \u00e9ruption du volcan de Santorini en 1950","volume":"13","author":"Georgalas","year":"1953","journal-title":"Bull. 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