Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/511
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dc.contributor.authorallTuvè, T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallTeramo, A.; Osservatorio Sismologico, Universita` di Messina, Messina, Italy.en
dc.contributor.authorallIbanez, J.; Instituto Andaluz de Geofisica, Universidad de Granada, Granada, Spainen
dc.contributor.authorallBottari, C.; Instituto Andaluz de Geofisica, Universidad de Granada, Granada, Spainen
dc.contributor.authorallTermini, D.; Osservatorio Sismologico, Universita` di Messina, Messina, Italy.en
dc.date.accessioned2005-10-31T17:33:13Zen
dc.date.available2005-10-31T17:33:13Zen
dc.date.issued2005-04en
dc.identifier.urihttp://hdl.handle.net/2122/511en
dc.description.abstractA modelling of the observed macroseismic intensity of historical and instrumental earthquakes in southern Spain is proposed, with the aim of determining the macroseismic parameters for seismic hazard evaluation in a region in which the characterization of intensity distribution of seismic events shows different levels of difficulty referable to the complex faults system of the area in study. The adopted procedure allows an analytical determination of epicenters and principal attenuation directions of earthquakes with a double level of verification with reference to the maximum shaking area and structural lineaments of the region, respectively. The analyses, carried out on a suitable number of events, highlight, therefore, some elements for a preliminary characterization of a seismic zonation on the basis of the consistency between seismic intensity distribution of earthquakes and corresponding structural framework.en
dc.format.extent523 bytesen
dc.format.extent477378 bytesen
dc.format.mimetypetext/htmlen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofPure and Applied Geophysicsen
dc.relation.ispartofseries4/162(2005)en
dc.subjectAttenuation directionsen
dc.subjectsouthern Spainen
dc.subjectmacroseismic intensityen
dc.subjectvirtual intensityen
dc.titleMacroseismic Intensity Modelling of Earthquakes in Southern Spain: Attenuation and Tectonic Implicationsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber747-760en
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.identifier.doi10.1007/s00024-004-2638-7en
dc.relation.referencesBLANCO, M.J. and SPAKMAN, W. (1993), The P-wave Velocity Structure in the Mantle below the Iberian Peninsula: Evidence for Subducted Lithosphere below Southern Spain, Tectonophysics 221, 13–34. BOCCALETTI, M., PAPANI, G., GELATI, R., RODRIGUEZ-FERNANDEZ, J., GARRIDO LOPEZ, A.C., and SANZ DE GALDEANO, C. (1987), Neogene-Quaternary Sedimentary-tectonic Evolution of the Betic Cordillera, Acta Naturalia de l’Ateneo Parmense 23, 179–200. BOTTARI, A., FEDERICO, B., and LO GIUDICE, E. (1984), The Correlation between the Macroseismic Attenuation Trend and the Geostructural Framework: The Calabro-Peloritanian Arc as an Example, Tectonophysics 108, 33–49. GALINDO-ZALDI´VAR, J., JABALOY, A., SERRANO, I., MORALES, J., GONZA´ LEZ-LODEIRO, F. and TORCAL, F. (1999), Recent and Present-day Stresses in the Granada Basin (Betic Cordilleras): Example of a Late Miocene-present-day Extensional Basin in a Convergent Plate Boundary, Tectonics 18, 686–702. GONZA´ LEZ-LODEIRO, F., ALDAYA, F., GALINDO-ZALDIVAR, J., and JABALOY, A. (1996), Superposition of Extensional Detachments during the Neogene in the Internal Zones of the Betic Cordilleras, Geol. Rundschare 85, 350–362. IBAN˜ EZ, J.M, BOTTARI, C, ESQUIVEL, J.A, MORALES, J., and ALGUACIL, G. (1999), Magnitude-intensity Relations for Instrumental and Historical (IX-XIX Century) Earthquakes in South Spain. Tectonical and Seismic Hazard Implications, Bull. Seismol. Soc. Am., still in preparation. LONERGAN, L. and WHITE, N., (1997), Origin of the Betic-Rift Mountain Belt, Tectonic 16, 504–522. LOPEZ-CASADO, C.,MOLINA-PALACIOS, S., DELGRADO J., and PELAEZ, J.A. (1999), Attenuation of Intensity with Epicentral Distance in the Iberian Penisula, still in preparation MEZCUA, J. (1982), Catalogo general de isosistas de la Penisula Iberica, Publicacio` n 202 IGN, Madrid. MORALES, J., SERRANO, I., JABALOY, A., GALINDO-ZALDIVAR, J., ZHAO, D., TORCAL, F., VIDAL, F., and GONZA´ LEZ-LODEIRO, F. (1999), Active Continental Subduction beneath the Betic Cordillera and the Albora´n Sea, Geology 27, 735–738. SANCHEZ NAVARRO NEUMAN, M. (1921), Lista de terremotos mas notables sentidos en la Penisula Iberica (a.C. 1917), Est. Sism. De Cartuja, 11–65. SANZ dE GALDEANO, C., LOPEZ CASADO, C., DELGADO, J., and PEINADO, M.A. (1995), Shallow Seismicity and Active Faults in the Betic Cordillera. A Preliminary Approach to Seismic Sources Associated with Specific Faults, Tectonophysics 248, 293–302. SEBER, D., BARAZANGI, M., IBERBRAHIM, A., and DEMNATI (1996), Geophysical Evidence for Lithospheric Delamination beneath the Albora´n Sea and Rif-Betic Mountains, Nature 379, 785–790. TERAMO, A., STILLITANI, E., and BOTTARI, A. (1995a), Anisotropic Characterization of Macroseismic Fields, Natural Hazard 11, 223–245. TERAMO, A., STILLITANI, E., and BOTTARI, A. (1995b), An Anisotropic Attenuation Law of the Macroseismic Intensity, Natural Hazard 11, 203–221. TERAMO, A., TERMINI, D., STILLITANI, E., and BOTTARI, A. (1996), The Determination of Epicentre by a Vectorial Modelling of Macroseismic Intensity Distribution, Natural Hazard 13, 101–117. TERMINI, D., BOTTARI, A., TERAMO, A., and TUVE` , T. (2005a), On the Observed Intensity Filtering in the Anisotropic Distribution Modelling of Macroseismic Intensity. Pure and Appl. Geophys. 162, 683–697 TERMINI, D., TERAMO, A., BOTTARI, C., and TUVE` , T. (2005b) An Anisotropic Attenuation Law of Macroseismic Intensity Performed on Virtual Intensity Distribution of Seismogenic Zones. Pure Appl. Geophys. 162, 707–714. TERMINI, D., BOTTARI, A., TERAMO, A., and BOTTARI, C. (2005c), On the Intensity Virtual Area Characterization in the Intensity Distribution Modelling by Macroseismic Planes, Pure Appl. Geophys. 162, 699–705. VISSERS, R.L.M., PLATT, J.P., and VAN DER WALD. (1995), Late Orogenic Extension of the Betic Cordillera and the Alboran domain: A Lithospheric View, Tectonics 14, 786–803. WEIJERMARS, R. (1985), Uplift and Subsidence History of the Alboran Basin and a Profile of the Alboran Diapir (W-Mediterranean), Geol. Mijnbouw 64, 349–356.en
dc.description.fulltextpartially_openen
dc.contributor.authorTuvè, T.en
dc.contributor.authorTeramo, A.en
dc.contributor.authorIbanez, J.en
dc.contributor.authorBottari, C.en
dc.contributor.authorTermini, D.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentOsservatorio Sismologico, Universita` di Messina, Messina, Italy.en
dc.contributor.departmentInstituto Andaluz de Geofisica, Universidad de Granada, Granada, Spainen
dc.contributor.departmentInstituto Andaluz de Geofisica, Universidad de Granada, Granada, Spainen
dc.contributor.departmentOsservatorio Sismologico, Universita` di Messina, Messina, Italy.en
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 OE, Catania, Italia-
crisitem.author.deptOsservatorio Sismologico, Università di Messina-
crisitem.author.deptInstituto Andaluz de Geofísica, University of Granada, Granada, Spain,-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptOsservatorio Sismologico, Universita` di Messina, Messina, Italy.-
crisitem.author.orcid0000-0003-4111-8008-
crisitem.author.orcid0000-0002-9846-8781-
crisitem.author.orcid0000-0003-4371-6060-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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-
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