Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5608
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dc.contributor.authorallTatevossian, R.; Institute of Physics of the Earth, RAS, Moscow, Russiaen
dc.contributor.authorallAlbini, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Milano-Pavia, Milano, Italiaen
dc.date.accessioned2010-01-14T13:08:05Zen
dc.date.available2010-01-14T13:08:05Zen
dc.date.issued2010-
dc.identifier.urihttp://hdl.handle.net/2122/5608en
dc.description.abstractEarthquake catalogues for Romania supply for 11th–15th century earthquakes located in the region of Vrancea records that consist of a complete set of parameters, including magnitude and depth. Scope of this paper is to verify the reliability and consistency of these parameters with the informative background as explicitly referenced by the catalogues. After retrieving the original sources they mention, the set of data appeared to be related almost exclusively to the Russian plain and too poor to be at the very origin of the parameter assessment. Data for 19th–20th century earthquakes, such as instrumental locations and CMT solutions, added to the understanding of the macroseismic response of the Russian plain to Vrancea earthquakes. On the one hand, the investigation and analysis of historical earthquake records for the fourteen events listed by the catalogues in the 11th–15th centuries has shown that for three earthquakes (1022, 1038, 1258) no primary sources could be traced, and three more earthquakes (1091, 1170 and 1328) are attested only by scarcely reliable records and had to be classified as doubtful, and one (1473) is simply a duplication of the 1471 event. On the other hand, the availability of data on recent earthquakes that may be compared to historical ones in terms of macroseismic effects allowed the authors to agree with the previous catalogue compilers’ solution with regard to both magnitude and depth of the past earthquakes for which do exist reliable primary historical records.en
dc.language.isoEnglishen_US
dc.publisher.nameSpringeren_US
dc.relation.ispartofNatural Hazardsen_US
dc.relation.ispartofseries/53 (2010)en_US
dc.subjectVrancea earthquakesen
dc.subject11th-15th earthquakesen
dc.titleInformation background of 11th-15th centuries earthquakes located by the current catalogues in Vrancea (Romania)en_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.type.QualityControlPeer-revieweden_US
dc.description.pagenumber575–604en_US
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.05. Historical seismologyen
dc.identifier.doi10.1007/s11069-009-9448-2en_US
dc.description.obiettivoSpecifico4IT. Banche datien_US
dc.description.journalTypeJCR Journalen_US
dc.description.fulltextopenen
dc.contributor.authorTatevossian, R.-
dc.contributor.authorAlbini, P.-
dc.contributor.departmentInstitute of Physics of the Earth, RAS, Moscow, Russiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italiaen_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptJoint Institute of Physics of the Earth, Russian Academy of Science, Moscow, Russia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia-
crisitem.author.orcid0000-0003-4149-9760-
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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