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9-3Šª
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1994”N
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E.43-E.48•Å
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PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM
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Kazuyoshi KUDO, Tsutomu SASATANI, Minoru SAKAUE, Seiji SAITO, Hideki NAGUMO, Masayoshi TAKAHASHI
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EFFECTS OF SURFACE SOIL AND EARTHQUAKE SOURCE RADIATION ON THE GROUND MOTION OF 1.6G ACCELERATION, OBSERVED DURING THE AUGUST 8,1993, SOUTH-WEST OFF HOKKAIDO EARTHQUAKE JAPAN.
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We examined the reasons why the ground motion of 1.6g was observed at OTB from the largest aftershock of the 1993 SW-Off Hokkaido earthquake. The strongest effect was a large amplification due to shallow surface soils overlying hard rock. The amplification factor relative to rock motion was around 40 at a resonance frequency and roughly 10 for maximum amplitude in time domain. In addition, a source radiation effect was also significant. SV-waves from this event predominated in the direction to OTB. It is also plausible that the source directivity contributed to the large amplitude at OTB.
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