Horizontal to vertical spectral ratio and geological conditions: an analysis of strong motion data from Greece and Taiwan (SMART-1)
- 1 January 1995
- journal article
- Published by Elsevier in Soil Dynamics and Earthquake Engineering
- Vol. 14 (3) , 177-197
- https://doi.org/10.1016/0267-7261(94)00039-j
Abstract
No abstract availableThis publication has 11 references indexed in Scilit:
- Site effect evaluation using spectral ratios with only one stationBulletin of the Seismological Society of America, 1993
- Field evaluation and site response identification at SMART-1 siteSoil Dynamics and Earthquake Engineering, 1992
- Dependence of strong ground motion on magnitude-distance, site geology and macroseismic intensity for shallow earthquakes in Greece: I, Peak horizontal acceleration, velocity and displacementSoil Dynamics and Earthquake Engineering, 1992
- Spatial coherency of shear waves from the Lotung, taiwan large-scale seismic testStructural Safety, 1991
- Spatial variability of seismic waves and its engineering applicationStructural Safety, 1991
- Characteristics of Strong Motion Durations in the SMART1 Array AreaTerrestrial, Atmospheric and Oceanic Sciences, 1991
- The SMART I Accelerograph Array (1980-1987): A ReviewEarthquake Spectra, 1987
- Dependence of sediment-filled valley response on input amplitude and valley propertiesBulletin of the Seismological Society of America, 1984
- Observed variations of earthquake motion across a sediment-filled valleyBulletin of the Seismological Society of America, 1984
- Observations of hard-rock site effectsBulletin of the Seismological Society of America, 1984