Spectral Strong Motion Attenuation in Central America

dc.creatorCliment Martín, Álvaro
dc.creatorTaylor Castillo, Waldo
dc.creatorCiudad Real, Mauricio
dc.creatorStrauch, Wilfred
dc.creatorSantana Barboza, Guillermo
dc.creatorVillagran, Mario
dc.creatorDahle, Anders
dc.creatorBungum, Hilmar
dc.date.accessioned2022-06-02T19:02:37Z
dc.date.accessioned2022-10-19T23:29:55Z
dc.date.available2022-06-02T19:02:37Z
dc.date.available2022-10-19T23:29:55Z
dc.date.created2022-06-02T19:02:37Z
dc.date.issued1994
dc.identifierhttps://hdl.handle.net/10669/86657
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4518415
dc.description.abstractA bayesian regression analysis of response spectral ordinates based on 218 digitized strong ground motion accelerograms (largest horizontal component) from Central America, augmented by 62 similar, high-magnitude observations from Guerrero, Mexico, has been performed using the simple linearized ground motion model: lnA = c1 + c2M + c3lnr +c4r = c5S + ln e where M is moment magnitude, r is hypocentral distance, S is zero for rock sites and 1 for soil sites and In£ is a normally distributed error term with zero mean and standard deviation sigma i.e. ln e = N (0, sigma) .
dc.languageeng
dc.relationSeismic Zonation and Earthquake Hazard Assessment;2-17
dc.sourceSpectral Strong Motion Attenuation in Central America(pp.1-49). The Research Council of Norway, Kjeller, Norway: NORSAR
dc.subjectStrong motion attenuation
dc.subjectCentral America
dc.subjectEARTHQUAKES
dc.titleSpectral Strong Motion Attenuation in Central America
dc.typereporte técnico


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