Analysis of Seismorgams in a Horizontal Array at Minami-Osaka Cite.
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概要
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Propagation of dominant later phases detected in the Osaka sedimentary basin are examined in this paper. We have maintained a tripartite array observation station in the Minami-Osaka site in the Senboku region, Osaka Pref. At the station, very important strong motion records were obtained from the 1995 Hyogo-Ken-Nanbu Earthquake. There were dominant later phases in the 90-120 seconds portion of NS trace and in the 45-75 seconds portion of EW trace. We conducted various examinations for the later phases to detect spectral characteristics, propagating direction, and phase velocities. As a result, we could clarified that the later phases mainly consisted of the Love wave from the Awaji Island direction.
- 公益社団法人 土木学会の論文
公益社団法人 土木学会 | 論文
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