Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3058
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dc.contributor.authorallScafidi, D.; Dipteris Università di Genovaen
dc.contributor.authorallMorasca, P.; Dipteris Università di Genovaen
dc.contributor.authorallSolarino, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallEva, C.; Dipteris Università di Genovaen
dc.date.accessioned2007-12-11T11:35:59Zen
dc.date.available2007-12-11T11:35:59Zen
dc.date.issued2007-10en
dc.identifier.urihttp://hdl.handle.net/2122/3058en
dc.description.abstractThe diverse studies carried out with geophysical and geodetic data in the last decades greatly improved the knowledge of the Alps-Apennines system. However, most of these studies were limited to portions of the system or to the shallow structures, and for these reasons reconstruction of the tectonic setting for a larger area and for the deeper layers is still open to different approaches and interpretations; in particular, very little is known about the deeper conjunction between the two chains. One of the most powerful tools to investigate the deeper part of an earth’s volume is seismic tomography. In fact, not only seismic tomography may reach depths that are far beyond those of many other methodologies, but it can provide information on very large areas (up to the entire earth) with a unique level of details. In this study, we applied diverse tomographic techniques to perform a multi-approach investigation on the crustal structure of the North-Western part of Italy, in particular to obtain the under surface velocity structure and the attenuation distribution. An accurate analysis of seismicity and focal mechanisms complemented the study. In the light of our new analysis of velocity tomography, attenuation tomography and focal mechanisms a more in deep interpretation of the characteristics of the Alps-Apennine system is now possible.en
dc.language.isoEnglishen
dc.relation.ispartofRendiconti della Società Geologica Italianaen
dc.relation.ispartofseries2 / 5 (2007)en
dc.subjectTomographyen
dc.subjectattenuationen
dc.titleA new deep picture of the Alps-Apennines system derived from seismological dataen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber211-213en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropyen
dc.relation.referencesCERMAK V., DELLA VEDOVA B., LUCAZEAU F., PASQUALE V., PELLIS G., SCHULTZ R. & VERDOYA M. (1992)- Heat flow density, in A Continent Revealed: the European Geotraverse, Edited by D. Blundell, R. Freeman and St. Mueller, Cambridge University Press, 1992. CAMPILLO M., FEIGNIER, B., BOUCHON M. & BÈTHOUX N. (1993) - Attenuation of Crustal Waves Across the Alpine Range. J. Geoph. Res. 98, B2, 1987-1996. CIACCIO M. G. & CHIARABBA C. (2002) - Tomographyc models and seismotectonics of the Reggio Emilia region, Italy. Tectonophysics 344, 261-276. DI STEFANO R., CHIARABBA C., LUCENTE F. & AMATO A. (1999) - Crustal and uppermost mantle structure in Italy from the inversion of P-wave arrival times: geodynamic implications. Geophys. J. Int. 139, 483-498. DOGLIONI C. (1993). Some remarks on the origin of foredeeps. Tectonophysics 228, 1–20 EVA C., CATTANEO M., AUGLIERA P., & Pasta, M. (1991) - Regional coda Q variations in the western Alps (northern Italy). Phys. Earth Planet. Inter. 67, 76-86. KISSLING E. (1993) - Deep structure of the Alps—what do we really know? Phys. Earth planet. Inter., 79, 87-112. PHILLIPS W. S., HARTSE H. E. & RUTLEDGE J. T. (2005) - Amplitude ratio tomography for regional phase Q. Geophys. Res. Lett., 32, no 21, L21301,doi: 10.1029/2005GL023870. ZHANG H., THURBER C.H., SHELLY D., IDE S., BEROZA, G. C. & HASEGAWA A., (2004) - High resolution subducting-slab structure beneath northern Honshu, Japan, revealed by double difference tomography, Geology, 32,4, 361-364.en
dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextpartially_openen
dc.contributor.authorScafidi, D.en
dc.contributor.authorMorasca, P.en
dc.contributor.authorSolarino, S.en
dc.contributor.authorEva, C.en
dc.contributor.departmentDipteris Università di Genovaen
dc.contributor.departmentDipteris Università di Genovaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentDipteris Università di Genovaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipTeRis Dipartimento per lo studio del territorio e delle sue risorse, Università di Genova-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptDipTeRis Dipartimento per lo studio del territorio e delle sue risorse, Università di Genova-
crisitem.author.orcid0000-0002-6525-4867-
crisitem.author.orcid0000-0002-9577-1347-
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-
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