Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2884
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dc.contributor.authorallCosta, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallMelnik, O.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallSparks, R. S. J.; Department of Earth Sciences, University of Bristol, Bristol, UK.en
dc.contributor.authorallVoight, B.; Geosciences, Penn State University, University Park, Pennsylvaniaen
dc.date.accessioned2007-11-29T08:09:02Zen
dc.date.available2007-11-29T08:09:02Zen
dc.date.issued2007en
dc.identifier.urihttp://hdl.handle.net/2122/2884en
dc.description.abstractLava dome eruptions are commonly characterized by large fluctuations in discharge rate with cyclic behaviour on time-scales ranging from hours to decades. Examples include Bezymianny volcano (Russia), Merapi (Java), Santiaguito (Guatemala), Mt St Helens (USA), Mt Unzen (Japan), and Soufrie`re Hills volcano (Montserrat). Previous models have assumed simple cylindrical conduits for magma transport, but extrusions are mainly fed by dykes, with cylindrical geometries developing only at shallow levels. The widths of dykes embedded in an elastic medium are influenced by local magma pressure, affecting flow rates and system dynamics strongly. We develop a model for magma flow in dykes, which predicts intense pulsations of magma extrusion for the case of a constant source pressure. The period time scale is determined by the elastic deformation of the dyke walls and the length-to-width ratio of the dyke. The dyke acts like a volumetric capacitor, storing magma as pressure increases and then releasing magma in a pulse of extrusion. For the Soufrie`re Hills volcano, cyclic extrusions with time-scales of a few weeks are predicted for dykes 300–500 m long and 3–6 m wide, matching observations. The model explains the sharp onset of tilt pulsations and seismic swarms.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeophisical Research Lettersen
dc.relation.ispartofseries/ 34 (2007)en
dc.subjectControlen
dc.subjectmagma flowen
dc.subjectdykesen
dc.subjectcyclic lavaen
dc.titleControl of magma flow in dykes on cyclic lava dome extrusionen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberL02303en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.03. Magmasen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.04. Thermodynamicsen
dc.identifier.doi10.1029/2006GL0227466en
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dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorCosta, A.en
dc.contributor.authorMelnik, O.en
dc.contributor.authorSparks, R. S. J.en
dc.contributor.authorVoight, B.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDepartment of Earth Sciences, University of Bristol, Bristol, UK.en
dc.contributor.departmentGeosciences, Penn State University, University Park, Pennsylvaniaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
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 Earth Sciences, University of Bristol, Bristol, UK.-
crisitem.author.deptDepartment of Geosciences, Penn State University, University Park, Pennsylvania, USA-
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.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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