Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2932
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dc.contributor.authorallCesca, S.; Inst. f. Geophysik, Uni Hamburgen
dc.contributor.authorallDahm, T.; Inst. f. Geophysik, Uni Hamburgen
dc.contributor.authorallBattaglia, J.; Laboratoire Magmas et Volcans, Toulouseen
dc.contributor.authorallBraun, T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2007-12-03T16:34:15Zen
dc.date.available2007-12-03T16:34:15Zen
dc.date.issued2007-03en
dc.identifier.urihttp://hdl.handle.net/2122/2932en
dc.description.abstractSource inversion for long period (LP) events in volcanic areas is an ongoing research topic. The high interest of volcanologists to understand the physical phenomena which govern these characteristic events is related to the fact that they may be directly generated by uid transfers and some of them could be candidates for volcanic activity parameters, or precursors of volcanic eruptions. The signal class of LP-type events generally includes di erent volcanic transients with dominant frequencies in the range between 0.5 and 5 Hz. Although some source models have been proposed to explain their generation (vibration of uid- lled cavities, etc.), the large variety of LP signal forms and the existence of alternative models to explain some of the observations, make it interesting to develop new inversion schemes. Our main goal is to propose an inversion methodology to determine LP source mechanisms and study these events through an exhaustive source inversion by using synthetic data.en
dc.language.isoEnglishen
dc.relation.ispartofDGG - German Geophysical Societyen
dc.subjectsource inversionen
dc.subjectvolcanoen
dc.titleFrequency domain inversion of synthetic long period volcanic eventsen
dc.typeOral presentationen
dc.description.statusPublisheden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismologyen
dc.description.ConferenceLocationBremen (Germany)en
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.fulltextopenen
dc.contributor.authorCesca, S.en
dc.contributor.authorDahm, T.en
dc.contributor.authorBattaglia, J.en
dc.contributor.authorBraun, T.en
dc.contributor.departmentInst. f. Geophysik, Uni Hamburgen
dc.contributor.departmentInst. f. Geophysik, Uni Hamburgen
dc.contributor.departmentLaboratoire Magmas et Volcans, Toulouseen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypeOral presentation-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptGFZ - Potsdam, Germany-
crisitem.author.deptGFZ Geoforschungszentrum Potsdam-
crisitem.author.deptDipartimento di Scienze Fisiche, Università degli Studi di Napoli Federico II-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-9513-1200-
crisitem.author.orcid0000-0003-1778-1328-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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