How to model amplification of strong earthquake motions by local soil and geologic site conditions
- 1 August 1990
- journal article
- research article
- Published by Wiley in Earthquake Engineering & Structural Dynamics
- Vol. 19 (6) , 833-846
- https://doi.org/10.1002/eqe.4290190605
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Frequency dependent attenuation of strong earthquake ground motionSoil Dynamics and Earthquake Engineering, 1990
- Empirical models for scaling pseudo relative velocity spectra of strong earthquake accelerations in terms of magnitude, distance, site intensity and recording site conditionsSoil Dynamics and Earthquake Engineering, 1989
- Empirical models for scaling Fourier amplitude spectra of strong ground acceleration in terms of earthquake magnitude source to station distance, site intensity and recording site conditionsSoil Dynamics and Earthquake Engineering, 1989
- A note on the noise amplitudes in some strong motion accelerographsSoil Dynamics and Earthquake Engineering, 1987
- Preliminary results from vertical seismic profiling of Oroville microearthquake S‐wavesGeophysical Research Letters, 1985
- Shallow shear wave velocity and Q structures at the El Centro strong motion accelerograph arrayGeophysical Research Letters, 1983
- Duration of strong earthquake shakingInternational Journal of Soil Dynamics and Earthquake Engineering, 1982
- Preliminary empirical model for scaling fourier amplitude spectra of strong ground acceleration in terms of modified mercalli intensity and recording site conditionsEarthquake Engineering & Structural Dynamics, 1979
- Scattering of plane sh waves by a semi‐elliptical canyonEarthquake Engineering & Structural Dynamics, 1974
- SEISMIC ATTENUATION OF GULF COAST SEDIMENTSGeophysics, 1969