Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2556
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dc.contributor.authorallPlomerová, J.; Geophysical Institute, Czech Acad. of Sci., Boční II, 141 31 Prague 4, Czech Republicen
dc.contributor.authorallMargheriti, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallPark, J.; Yale University, Department of Geology and Geophysics, New Haven, USAen
dc.contributor.authorallBabuška, V.; Geophysical Institute, Czech Acad. of Sci., Boční II, 141 31 Prague 4, Czech Republicen
dc.contributor.authorallPondrelli, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallVecsey, L.; Rutgers University, Department of Geological Sciences, NJ, USAen
dc.contributor.authorallPiccinini, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallLevin, L.; Rutgers University, Department of Geological Sciences, NJ, USAen
dc.contributor.authorallBaccheschi, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallSalimbeni, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.date.accessioned2007-10-08T13:27:37Zen
dc.date.available2007-10-08T13:27:37Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2556en
dc.description.abstractShear-wave splitting estimates from recordings of 10 portable seismographic stations during the first year of the RETREAT seismic deployment, in combination with broadband data from the Italian national seismic network, are associated with seismic anisotropy within the upper mantle beneath the Northern Apennines. Anisotropic parameters derived from both shear-wave splitting and P travel-time residuals vary geographically and depend on event back-azimuth, reflecting complexity in the underlying mantle strain field. Variations of the splitting time delays and fast polarization seem to exclude a 2-D sublithosphere corner flow, associated with the Apennines subduction, as the main source of the inferred anisotropy. The anisotropic signal may be generated by a frozen-in fabric of the Adriatic and Tyrrhenian lithosphere domains, or by flow variations induced by episodic and fragmentary slab rollback.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofEarth Planet. Sci. Lett.en
dc.relation.ispartofseries/ 247 (2006)en
dc.subjectbirefringence;en
dc.subjectApenninesen
dc.titleSeismic anisotropy beneath the Northern Apennines (Italy): Mantle flow or lithosphere fabric?en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber157-170en
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processesen
dc.identifier.doi10.1016/j.epsl.2006.04.023en
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dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorPlomerová, J.en
dc.contributor.authorMargheriti, L.en
dc.contributor.authorPark, J.en
dc.contributor.authorBabuška, V.en
dc.contributor.authorPondrelli, S.en
dc.contributor.authorVecsey, L.en
dc.contributor.authorPiccinini, D.en
dc.contributor.authorLevin, L.en
dc.contributor.authorBaccheschi, P.en
dc.contributor.authorSalimbeni, S.en
dc.contributor.departmentGeophysical Institute, Czech Acad. of Sci., Boční II, 141 31 Prague 4, Czech Republicen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentYale University, Department of Geology and Geophysics, New Haven, USAen
dc.contributor.departmentGeophysical Institute, Czech Acad. of Sci., Boční II, 141 31 Prague 4, Czech Republicen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentRutgers University, Department of Geological Sciences, NJ, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentRutgers University, Department of Geological Sciences, NJ, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
item.openairetypearticle-
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
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crisitem.author.deptGeophysical Institute, Czech Academy of Sciences, Czech Republic-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptYale University, Dept. of Geology and Geophysics, New Haven, USA-
crisitem.author.deptGeophysical Institute, Czech Academy of Sciences, Prague, Czech Republic-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptGeophysical Institute, Czech Academy of Sciences, Czech Republic-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptRutgers University, Department of Geological Sciences, Piscataway, NJ, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0003-3853-254X-
crisitem.author.orcid0000-0002-2117-7118-
crisitem.author.orcid0000-0002-0851-7405-
crisitem.author.orcid0000-0002-1826-646X-
crisitem.author.orcid0000-0001-5383-7945-
crisitem.author.orcid0000-0002-1077-5833-
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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