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VolF10-1Šª
”NF 1998”N
•ÅF 559-564•Å
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ŒfÚŽGŽi‰pjF THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
’˜ŽÒi‰pjF Takumi TOSHINAWA,Rafael RIDDELL,Ernesto CRUZ,Francisco GAJARDO
ƒ^ƒCƒgƒ‹i‰pjF EVALUATION OF THE DISTRIBUTION OF GROUND-MOTION CHARACTERISTICS IN SANTIAGO, CHILE
´˜^i‰pjF In Santiago, Chile, strong-motion array observation has been conducted since 1989. Observed accelerograms show that a silty-soil site has the largest amplification characteristics among the sites. To evaluate the distribution of ground-motion characteristics around the silty-soil site, dense microtremor observation was carried out. Horizontal to vertical spectral ratios of microtremors were obtained for 69 sites. Fundamental periods of H/V spectral ratios were correlated with the thickness of Pleistocene deposits. Plural spectral peaks in the northern part of the area suggest the existence of soft subsurface soils on the Pleistocene deposits. High maximum spectral peak values in the northeastern part of the area suggest the possibility of high amplification during earthquakes.
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