�@ Œf�ÚŽGŽ��i˜a�j�F “ú–{’n�k�HŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶�W Vol�F 9-3Šª ”N�F 1994”N •Å�F E.121-E.126•Å ’˜ŽÒ�i˜a�j�F - ƒ^ƒCƒgƒ‹�i˜a�j�F - �´˜^�i˜a�j�F
- ƒL�[ƒ��[ƒh�i˜a�j�F - Œf�ÚŽGŽ��i‰p�j�F PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒ�i‰p�j�F Masahiro IIDA, Mario ORDAZ, Hitoshi TANIGUCHI, Carlos GUTIERREZ, Miguel SANTOYO ƒ^ƒCƒgƒ‹�i‰p�j�F INTERPRETATION OF WAVE FIELD INSIDE THE MEXICO VALLEY ON THE BASIS OF BOREHOLE DATA �´˜^�i‰p�j�F
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. ƒL�[ƒ��[ƒh�i‰p�j�F - ‹LŽ–‹æ•ª�F - ‹æ•ª �@�@�@ˆÏˆõ‰ï˜_•¶�W