Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5401
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dc.contributor.authorallHautmann, S.; Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdomen
dc.contributor.authorallGottsmann, J.; Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdomen
dc.contributor.authorallSparks, R. S. J.; Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdomen
dc.contributor.authorallCosta, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallMelnik, O.; Institute of Mechanics, Moscow State University, 1-112b Michurinsky prosp., Moscow, Russiaen
dc.contributor.authorallVoight, B.; Department of Geosciences, Penn State University, 334A Deike Building, University Park, PA 16802, USAen
dc.date.accessioned2009-12-30T07:13:55Zen
dc.date.available2009-12-30T07:13:55Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5401en
dc.description.abstractA dyke conduit has been shown to be a realistic model for the shallow magmatic feeder system for the dome forming eruption at Soufrière Hills Volcano, Montserrat. Here we use a three-dimensional Finite Element model to examine the ground deformation that can be expected due to the pressurization of a dyke conduit. We find that the generated deformation has a bilateral symmetry with nearly no displacement in the direction of dyke strike, and a maximal ground deformation about 1 km away from the vent in the perpendicular direction. Resultant surface deformation is mainly triggered by the upper part of the feeder system, where the dyke opens into a cylindrical conduit. We apply our deformation model to investigate tilt data collected in 1997 in order to infer the orientation of the dyke. We obtain a best-fit for a NNW–SSE trending dyke, which matches observations of the ground displacement field obtained by differential GPS and the alignment of main structural geologic features of southern Montserrat.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofTectonophysicsen
dc.relation.ispartofseries/471 (2009)en
dc.subjectSoufrière Hills Volcanoen
dc.subjectDyke conduiten
dc.subjectFinite Element Modelen
dc.subjectGround deformationen
dc.titleModelling ground deformation caused by oscillating overpressure in a dyke conduit at Soufrière Hills Volcano, Montserraten
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber87–95en
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.08. Volcanic arcsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.03. Inverse methodsen
dc.identifier.doi10.1016/j.tecto.2008.10.021en
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dc.description.obiettivoSpecifico3.5. Geologia e storia dei vulcani ed evoluzione dei magmien
dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorHautmann, S.en
dc.contributor.authorGottsmann, J.en
dc.contributor.authorSparks, R. S. J.en
dc.contributor.authorCosta, A.en
dc.contributor.authorMelnik, O.en
dc.contributor.authorVoight, B.en
dc.contributor.departmentDepartment of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdomen
dc.contributor.departmentDepartment of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdomen
dc.contributor.departmentDepartment of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdomen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentInstitute of Mechanics, Moscow State University, 1-112b Michurinsky prosp., Moscow, Russiaen
dc.contributor.departmentDepartment of Geosciences, Penn State University, 334A Deike Building, University Park, PA 16802, USAen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdom-
crisitem.author.deptBristol University-
crisitem.author.deptDepartment of Earth Sciences, University of Bristol, Bristol, UK.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptInst. Mechanics, Moscow State University, Moskow, Russia-
crisitem.author.deptDepartment of Geosciences, Penn State University, University Park, Pennsylvania, USA-
crisitem.author.orcid0000-0001-9280-4011-
crisitem.author.orcid0000-0002-4987-6471-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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