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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10201
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dc.contributor.authorallGiammanco, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallGladys, M.; Environmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.contributor.authorallNeri, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallHernández, P.; Environmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.contributor.authorallSortino, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallBarrancos, J.; Environmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.contributor.authorallLópez, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallPecoraino, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallPerez, N.; Environmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.date.accessioned2016-02-03T08:28:12Zen
dc.date.available2016-02-03T08:28:12Zen
dc.date.issued2016en
dc.identifier.urihttp://hdl.handle.net/2122/10201en
dc.description.abstractThis work presents the results of an extensive geochemical survey aimed at measuring soil CO2 effluxes and soil temperatures over a large portion of Mt. Etna's summit area, coupled with an updated structural survey of the same area. The main goals of this study were i) to find concealed or hidden volcano-tectonic structures in the studied area by detecting anomalous soil gas emissions, ii) to investigate the origin of the emitted gas and the mechanism of gas and heat transport to the surface, iii) to produce a structural model based both on the surface geology and on the soil gas data and, lastly, iv) to contribute to the assessment of hazard from slope failure and crater collapses at Mt. Etna. The results revealed many concealed structural lines that followed the major directions of structural weakness in the summit area of Mt. Etna, mostly due to a combined action of gravitational spreading of the volcano and magma intrusions. Both recent and old volcano-tectonic lines were found to act as pathways for the leakage of magmatic gases to the surface. An important role in driving magmatic gases to the surface is also played by fracturing and faulting due to caldera-forming collapses and smaller crater collapses. Correlation between soil CO2 emissions and soil temperature allowed discriminating areas of active shallow hydrothermal circulation along deep fractures (characterized by high values of both parameters, but mostly soil temperature) from those affected by undeveloped fractures that did not reach the surface (characterized by high CO2 emissions at low temperature). The former corresponded to weak zones of the volcano edifice that were frequently site of past eruptions, indicating that those areas keep a high potential for future opening of eruptive fissures. The latter were likely related to sites where new eruptive fissures may open in the near future due to backward propagation of extensional tectonic stress.en
dc.description.sponsorshipproject CGL2005-07509/CLI, Ministry of Education and Science of Spain; DPC-INGV project FLANK; Istituto Nazionale di Geofisica e Vulcanologia — Osservatorio Etneo, Sezione di Cataniaen
dc.language.isoEnglishen
dc.publisher.nameElsevier Science Limiteden
dc.relation.ispartofJournal of volcanology and geothermal researchen
dc.relation.ispartofseries/311 (2016)en
dc.subjectMt. Etnaen
dc.subjectSoil CO2en
dc.subjectSoil temperatureen
dc.subjectHidden faultsen
dc.subjectStructural frameworken
dc.titleActive tectonic features and structural dynamics of the summit area of Mt. Etna (Italy) revealed by soil CO2 and soil temperature surveyingen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber79-98en
dc.identifier.URLhttp://www.sciencedirect.com/science/article/pii/S0377027316000068en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.01. Gasesen
dc.identifier.doi10.1016/j.jvolgeores.2016.01.004en
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dc.description.obiettivoSpecifico5A. Energia e georisorseen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0377-0273en
dc.relation.eissn1872-6097en
dc.contributor.authorGiammanco, S.en
dc.contributor.authorGladys, M.en
dc.contributor.authorNeri, M.en
dc.contributor.authorHernández, P.en
dc.contributor.authorSortino, F.en
dc.contributor.authorBarrancos, J.en
dc.contributor.authorLópez, M.en
dc.contributor.authorPecoraino, G.en
dc.contributor.authorPerez, N.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentEnvironmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentEnvironmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentEnvironmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentEnvironmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spainen
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crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptEnvironmental Research Division, Instituto Tecnológico y de Energías Renovables (ITER), Spain-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.orcid0000-0003-2588-1441-
crisitem.author.orcid0000-0002-5890-3398-
crisitem.author.orcid0000-0003-4707-515X-
crisitem.author.orcid0000-0002-2400-911X-
crisitem.author.orcid0000-0001-5478-1912-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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