1991
DOI: 10.3133/ofr91441h
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Engineering characterization of earthquake strong ground motions with applications to the Pacific Northwest

Abstract: This paper is one of a series dealing with earthquake hazards of the Pacific Northwest, primarily in western Oregon and western Washington. This research represents the efforts of U.S. Geological Survey, university, and industry scientists in response to the Survey initiatives under the National Earthquake Hazards Reduction Program. Subject to Director's approval, these papers will appear collectively as U.S. Geological Survey Professional Paper 1560, tentatively titled "Assessing and Reducing Earthquake Hazar… Show more

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Cited by 32 publications
(47 citation statements)
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“…to two alternative simulations; these are the ground-motion relations for the Brune (single-corner-frequency) 80-bar source model (as described earlier), and the stochastic finitefault simulations made using the alternative methodology of Silva et al (1990). The stochastic simulations of Silva et al are very similar in concept to those presented here, but were generated using somewhat different assumptions regarding fault dimensions, subfault size, rise time, and attenuation, as described by Schneider et al (1993).…”
Section: Comparison Of Ground Motion Relations To California Databasementioning
confidence: 80%
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“…to two alternative simulations; these are the ground-motion relations for the Brune (single-corner-frequency) 80-bar source model (as described earlier), and the stochastic finitefault simulations made using the alternative methodology of Silva et al (1990). The stochastic simulations of Silva et al are very similar in concept to those presented here, but were generated using somewhat different assumptions regarding fault dimensions, subfault size, rise time, and attenuation, as described by Schneider et al (1993).…”
Section: Comparison Of Ground Motion Relations To California Databasementioning
confidence: 80%
“…They agree well with empirical regression equations (e.g., Abrahamson and Silva, 1997;Sadigh et al, 1997) in the magnitude-distance ranges that are well represented by the strong-motion database. The stochastic ground motion relations are underpinned by a source model that has been validated for earthquakes from magnitudes 4 through 8 (e.g., Silva et al, 1990;Schneider et al, 1993;Silva and Darragh, 1995;Beresnev and Atkinson, 1997, 1998a, 1998b. The attenuation model is derived from regional seismographic data over distances of hundreds of km (Raoof et al, 1999).…”
Section: Discussionmentioning
confidence: 99%
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