Seismic microzoning of Belgrade

• Published in: Soil dynamics and earthquake engineering (1984) Vol. 97; pp. 395 - 412
• Main Authors: Lee, V.W., Trifunac, M.D., Bulajić, B.Đ., Manić, M.I., Herak, D., Herak, M.
• Format: Journal Article
• Language: English
• Published: Barking Elsevier Ltd 01-06-2017; Elsevier BV
• Subjects: Amplitudes; Computation of seismic hazard for earthquake sources that follow different attenuation laws; Contribution of a large distant earthquake to the design strong motion amplitudes; Design; Design standards; Earthquakes; Geology; Ground motion; Microzonation maps, which include a description of site geology and site soil properties; Nonlinear response; Scaling; Seismic activity; Seismic design; Seismic engineering; Soil classification; Soil properties; Spatial analysis; Spatial distribution; Studies; Belgrade Serbia; Contribution of a large distant earthquake to the design strong motion amplitudes; Computation of seismic hazard for earthquake sources that follow different attenuation laws; Microzonation maps, which include a description of site geology and site soil properties
• ISSN: 0267-7261; 1879-341X
• DOI: 10.1016/j.soildyn.2017.02.002

Seismic microzonation maps for Belgrade (Serbia) and its surroundings are presented based on the uniform-hazard-spectrum (UHS) methodology. Such mapping must satisfy the guidelines for performance-based design (PBD), which at present requires the specification of two sets of spectral amplitudes, one in which the structure would remain essentially linear, and one in which it would undergo nonlinear response. These requirements cannot be achieved by specifying the design spectra using only one (same) fixed spectral shape, and such spectra cannot be scaled by the peak ground acceleration alone. Another source of difficulties in the selection of the design amplitudes for PBD occurs when the standard spectrum shape is not capable of describing excitation by large, distant earthquakes. Furthermore, scaling the site dependent design ground motion only via soil site classification ignores the effects of site geology and thus leads to biased results. The maps we present in this paper avoid these shortcomings and include the effects of near and distant large earthquakes, spatial distribution of seismic activity, site geology, and site soil properties in a balanced way.