Titlebook: Earthquake Microzoning; Antoni Roca (Head of the Geological Survey),Carlos Book 2002 Springer Basel AG 2002 Earthquake mechanism.earthquak

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Microzonation of Lisbon: 1-D Theoretical Approach,s and laboratory tests. The results are presented as contour maps for the peak frequencies and for the corresponding amplification factors. These results are compared with the microzonation map obtained by microtremor analysis and with the damage distribution observed in past earthquakes.

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2504-3625 he theoretical/numerical 1-D and 2-D modelling methods. Additional contributions discussing techniques for characterising soil properties, microzoning applications to several urban areas, and others were added to the volume to broaden this important topic.978-3-7643-6652-0978-3-0348-8177-7Series ISSN 2504-3625 Series E-ISSN 2504-3633

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Panos J. Antsaklis,Anthony N. Micheltional amplification in response spectra that cannot be accounted for without reference to the lateral heterogeneity of the valley structure. Our numerical results are extensively compared with observations, which show that the additional amplification computed from the 2-D model is real and affects

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M. L. Mallory,L. L. Loseto,S. H. Ferguson the finite-difference method. We compare the results of the two simulations, both in the time and frequency domain. We also compare the results with experimental data related to an event recorded by the Reftek network installed in the target area. This permits a better understanding of how the stru

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A Logical Introduction to Proofmponent ., while the radial . and vertical (V) components are sensitive to the scenario earthquake. Although the strongest local effects affect the . component, both observed and synthetic, a complete determination of the seismic input for the built environment requires the knowledge of all three co

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A Longitudinal Study of DyslexiaRatio (SBSR) and with the Horizontal Component (HC) of the transfer function for the displacement at the same locations. The comparison shows that, in general, HVSR cannot provide the . period of a site due to the fact that this technique cannot predict accurately the Spectral amplification levels.

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