Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5300
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dc.contributor.authorallMartinez-Arévalo, C.; Museo Nacional de Ciencias Naturales. CSIC, Madriden
dc.contributor.authorallMusumeci, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallPatanè, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.date.accessioned2009-12-02T08:28:41Zen
dc.date.available2009-12-02T08:28:41Zen
dc.date.issued2009-07-01en
dc.identifier.urihttp://hdl.handle.net/2122/5300en
dc.description.abstractTeleseismic body waves from broadband seismic stations are used to investigate the crustal and uppermost mantle structure of Stromboli volcano through inversion of the receiver functions (RFs). First, we computed RFs in the frequency domain using a multiple-taper spectral correlation technique. Then, the nonlinear neighbourhood algorithm was applied to estimate the seismic shear wave velocity of the crust and uppermost mantle and to define the main seismic velocity discontinuities. The stability of the inversion solution was tested using a range of initial random seeds and model parameterizations. A shallow Moho, present at depth of 14.8 km, is evidence of a thinned crust beneath Stromboli volcano. However, the most intriguing and innovative result is a low S velocity layer in the uppermost mantle, below 32 km. The low S velocity layer suggests a possible partial melt region associated with the volcanism, as also recently supported by tomographic studies and petrological estimations.en
dc.language.isoEnglishen
dc.relation.ispartofTerra Novaen
dc.relation.ispartofseries/21 (2009)en
dc.subjectreceiver functionen
dc.subjectStrombolien
dc.titleEvidence of a partial melt zone beneath Stromboli volcano (Italy) from inversion of teleseismic receiver functionsen
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber386-392en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismologyen
dc.identifier.doi10.1111/j.1365-3121.2009.00894.xen
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dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorMartinez-Arévalo, C.en
dc.contributor.authorMusumeci, C.en
dc.contributor.authorPatanè, D.en
dc.contributor.departmentMuseo Nacional de Ciencias Naturales. CSIC, Madriden
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartamento de Volcanología, Museo Nacional de Ciencias Naturales, CSIC, Madrid Spain-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0002-0143-4594-
crisitem.author.orcid0000-0001-9410-5126-
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-
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