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9-3Šª
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1994”N
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E.121-E.126•Å
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PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM
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Masahiro IIDA, Mario ORDAZ, Hitoshi TANIGUCHI, Carlos GUTIERREZ, Miguel SANTOYO
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INTERPRETATION OF WAVE FIELD INSIDE THE MEXICO VALLEY ON THE BASIS OF BOREHOLE DATA
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During the 1985 Michoacan earthquake (Ms=8.1), seismic waves were amazingly amplified in the lakebed zone of Mexico City, which is approximately 400 km from the epicenter, and the long duration of the lakebed seismograms was a real surprise. In the present study, we hypothesize that the long coda is not only surface waves, but also long-period body waves, which are produced by the multipathing due to the long-distance path and the very soft surficial layers. We perform the nonstationary spectrum analysis, the 1-D elastic propagation analysis and the cross correlation analysis for borehole data at lakebed stations. These analyses indicate that the soft surficial layers afford to cause dominant-period waves, and that the long-duration records are composed of both surface waves and long-period body waves.
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