Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2525
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dc.contributor.authorallStrasser, F. O.; Department of Civil & Environmental Engineering Imperial College Londonen
dc.contributor.authorallMontaldo, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Milano-Pavia, Milano, Italiaen
dc.contributor.authorallDouglas, J.; BRGM, ARN/RISen
dc.contributor.authorallBommer, J. J.; Department of Civil & Environmental Engineering Imperial College Londonen
dc.date.accessioned2007-09-20T12:14:47Zen
dc.date.available2007-09-20T12:14:47Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2525en
dc.description.abstractThe influence of style-of-faulting on strong groundmotions has been the subject of debate for some time. Although some controversy persists, the general consensus is that ground motions produced by reverse faults are higher than those produced by normal faults, whereas motions from strike-slip faults are somewhere in between. In a recent article, Convertito and Herrero (2004) derived a correction factor for focal mechanism to be applied to predictive equations. This issue was previously addressed by Bommer et al. (2003). Although this article is cited by Convertito and Herrero, it seems that its aims and scope were not well understood, and we would therefore like to clarify what the method presented therein entails, especially because we feel that Convertito and Herrero’s approach of characterizing focal mechanisms based solely on the radiation pattern is difficult to justify. After presenting their correction scheme, Convertito and Herrero go on to present an implementation of probabilistic seismic hazard analysis (PSHA) explicitly accounting for focal mechanism. This represents a real innovation in terms of methodology because it allows propagation of the improvements in ground-motion prediction gained through the focal-mechanism adjustments to hazard estimation. Characterizing the dominant scenario in terms of focal mechanism furthermore has the advantage of providing constraints for numerical simulations that are derived directly from the hazard computation, rather than from arbitrary assumptions. However, in our opinion, the methodology presented by Convertito and Herrero has some serious shortcomings which would need to be addressed before it can lead to improvements of the PSHA methodology. Our discussion includes a comparison with the new Italian seismic hazard map, which was derived using the Bommer et al. (2003) adjustment methodology.en
dc.language.isoEnglishen
dc.publisher.nameSeismological Society of Americaen
dc.relation.ispartofBull. Seismol. Soc. Amer.en
dc.relation.ispartofseries2 / 96 (2006)en
dc.subjectstrong ground-motionsen
dc.titleComment on "Influence of fochal mechanism in probabilistic seismic hazard analysis" by Vincenzo Convertito and Andre' Herreroen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber750-753en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.identifier.doi10.1785/0120050101en
dc.relation.referencesAbrahamson, N. A., P. Birkhauser, M. Koller, D. Mayer-Rosa, P. Smit, C. Sprecher, S. Tinic, and R. Graf (2002). Pegasos—a comprehensive probabilistic seismic hazard assessment for nuclear power plants in Switzerland, presented at the 12th European Conference on Earthquake Engineering, London, paper no. 633. Ambraseys, N. N., J. Douglas, S. K. Sarma, and P. M. Smit (2005). Equations for the estimation of strong ground motions from shallow crustal earthquakes using data from Europe and the Middle East: horizontal peak ground acceleration and spectral acceleration, Bull. Earthquake Eng. 3, no. 1, 1–53. Ambraseys, N. N., K. A. Simpson, and J. J. Bommer (1996). The prediction of horizontal response spectra in Europe, Earthquake Eng. Struct. Dyn. 25, no. 4, 371–400. Boore, D. M., and J. Boatwright (1984). Average body-wave radiation coefficients, Bull. Seism. Soc. Am. 74, no. 5, 1615–1621. Boore, D. M., W. B. Joyner, and T. Fumal (1997). Equations for estimating horizontal response spectra and peak acceleration from western North American earthquakes: a summary of recent work, Seism. Res. Lett. 68, no. 1, 128–153. Bommer, J. J., J. Douglas, and F. O. Strasser (2003). Style-of-faulting in ground-motion prediction equations, Bull. Earthquake Eng. 1, no. 2, 171–202. Bommer, J., F. Scherbaum, H. Bungum, F. Cotton, F. Sabetta, and N. Abrahamson (2005). On the use of logic-trees for ground-motion prediction equations in seismic-hazard analysis, Bull. Seism. Soc. Am. 95, no. 2, 377–389. Campbell, K. W. (1997). Empirical near-source attenuation relationships for horizontal and vertical components of peak ground acceleration, peak ground velocity, and pseudo-absolute acceleration response spectra, Seism. Res. Lett. 68, no. 1, 154–179. Campbell, K. W. (2003). Prediction of strong ground motion using the hybrid empirical method: example application to eastern North America, Bull. Seism. Soc. Am. 93, no. 3, 1012–1033. Convertito, V., and A. Herrero (2004). Influence of focal mechanism in probabilistic seismic hazard analysis, Bull. Seism. Soc. Am. 94, no. 6, 2124–2136. Cotton, F., F. Scherbaum, J. J. Bommer, and H. Bungum (2006). Criteria for selecting and adjusting ground-motion models for specific target regions (in press). Gruppo di Lavoro MPS (2004). Redazione della mappa di pericolosita` sismica prevista dall’Ordinanza PCM 3274 del 20 marzo 2003. Rapporto Conclusivo per il Dipartimento della Protezione Civile, INGV, Milano-Roma, April 2004, 65 pp. 5 annexes. http://zonesismiche. mi.ingv.it/documenti/rapporto_conclusivo.pdf (in Italian). Jackson, J. (2001). Living with earthquakes: know your faults. The 5th Mallet-Milne Lecture, J. Earthquake Eng. 5, Special Issue 1, 5–123. McGarr, A. (1984). Scaling of ground-motion parameters, state of stress and focal depth, J. Geophys. Res. 89, no. B10, 6969–6979. Montaldo, V., E. Faccioli, A. Akinci, L. Malagnini, and G. Zonno (2005). Treatment of ground-motion predictive relationships for the reference seismic hazard map of Italy, J. Seism. 9, no. 3, 295–316. Sabetta, F., and A. Pugliese (1987). Attenuation of peak horizontal acceleration and velocity from Italian strong-motion records, Bull. Seism. Soc. Am. 77, no. 5, 1491–1513. Sabetta, F., and A. Pugliese (1996). Estimation of response spectra and simulation of nonstationary earthquake ground motions, Bull. Seism. Soc. Am. 86, no. 2, 337–352. Spudich, P., W. B. Joyner, A. G. Lindh, D. M. Boore, B. M. Margaris, and J. B. Fletcher (1999). SEA99: revised ground motion prediction relation for use in extensional tectonic regimes, Bull. Seism. Soc. Am. 89, no. 5, 1156–1170.en
dc.source.commentaryonConvertito, V., and A. Herrero (2004). Influence of focal mechanism in probabilistic seismic hazard analysis, Bull. Seism. Soc. Am. 94, no. 6, 2124–2136.en
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorStrasser, F. O.en
dc.contributor.authorMontaldo, V.en
dc.contributor.authorDouglas, J.en
dc.contributor.authorBommer, J. J.en
dc.contributor.departmentDepartment of Civil & Environmental Engineering Imperial College Londonen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italiaen
dc.contributor.departmentBRGM, ARN/RISen
dc.contributor.departmentDepartment of Civil & Environmental Engineering Imperial College Londonen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCouncil for Geoscience-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia-
crisitem.author.deptBRGM, Orléans, France-
crisitem.author.deptImperial College London, Civil & Environmental Engineering, London SW7 2AZ, UK-
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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