1991
DOI: 10.1016/0040-1951(91)90201-3
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Some ideas for a databank of macroseismic data

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Cited by 5 publications
(3 citation statements)
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“…Grandori and Faccioli also defined a horizontal response spectrum to be used as seismic input for dynamic analyses. The spectrum was obtained by enveloping the horizontal response spectra of actual recorded accelerograms extracted from a database of Italian earthquakes available at the time (Postpischl et al 1991). The selection of the accelerograms was performed by considering magnitudes between 5.4 and 6.8, distances from the source between 24 and 53 km, and the geotechnical/ geological conditions of the site.…”
Section: Previous Studies Of Seismic Inputmentioning
confidence: 99%
“…Grandori and Faccioli also defined a horizontal response spectrum to be used as seismic input for dynamic analyses. The spectrum was obtained by enveloping the horizontal response spectra of actual recorded accelerograms extracted from a database of Italian earthquakes available at the time (Postpischl et al 1991). The selection of the accelerograms was performed by considering magnitudes between 5.4 and 6.8, distances from the source between 24 and 53 km, and the geotechnical/ geological conditions of the site.…”
Section: Previous Studies Of Seismic Inputmentioning
confidence: 99%
“…Historical seismology is not new to the use of advanced solutions for organizing archives of historical data (Godefroy et al 1990;Postpischl et al 1991;Boschi et al 1996), but some time has passed since a new experimental attempt was conducted in the field. The core of this research work is to review how historical seismologists deal with the various data types retrieved in their historical research process, map their relations, and to design a tool able to support the entire research process.…”
Section: Introductionmentioning
confidence: 99%
“…La macrosísmica conduce al conocimiento de las particularidades fenomenológicas de los terremotos, en especial los parámetros de localización hipocentral, zonas de daños, extensión horizontal y vertical de la ruptura, mecanismo focal, momento sísmico y la atenuación de la intensidad(Salcedo, 2002). De esta forma, estos estudios generan datos e información que tienen carácter de complementariedad frente a los datos instrumentales; de manera que con ellos también se alimentan los catálogos sísmicos de una región sismoactiva(Postpischl et al, 1991).En su mayoría, los sismos ocurridos en periodos preinstrumentales resultan ser de mayor intensidad que los recientes, por lo cual en muchas regiones del mundo no se conocen los sismos grandes que las han afectado, quedando un vacío substancial en el conocimiento sísmico de las grandes intensidades y su periodo de retorno, lo que dificulta la evaluación confiable del peligro sísmico(Guidoboni and Stucchi, 1993).Entonces, de los estudios macrosísmicos sobre un terremotos particular se espera el aporte en la determinación de parámetros sismológicos que llenen el vacío que tiene los catálogos por la carencia de redes sísmicas o por el corto periodo de registro instrumental. Con este propósito se llevó a cabo este estudio que presenta datos sismológicos relevantes para la interpretación del área de…”
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