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Observations were made on a line running in the north-south direction from Kawachinagano, Osaka Prefecture to Kiwa, Mie Prefecture. The line crosses major geological zones which characterize the geological features of southwestern Japan. Six shots were fired and the generated seismic waves were recorded at 86 temporary observation sites. High quality records were obtained for all shots despite rainy weather on the second day of the experiment. Very prominent later arrivals, probably reflected waves from the lower crust or the upper mantle, can be recognized on the record sections. Travel times of the first arrival suggest rather gentle structure in the upper crust. Results of the detailed analysis showing the structure from the upper crust to the upper mantle beneath the Kii Peninsula will be published in a separate paper.","subitem_description_type":"Abstract"},{"subitem_description":"1998\u5e7411\u670817\u65e5\u304a\u3088\u307318\u65e5\u306e\u65e9\u671d,\u7d00\u4f0a\u534a\u5cf6\u5185\u306e\u5927\u962a\u5e9c\u6cb3\u5185\u9577\u91ce\u5e02\u3068\u4e09\u91cd\u770c\u7d00\u548c\u753a\u3092\u7d50\u3076\u5168\u9577\u7d0465km\u306e\u6e2c\u7dda\u3067,\u4eba\u5de5\u5730\u9707\u306b\u3088\u308b\u5730\u4e0b\u69cb\u9020\u8abf\u67fb\u304c\u884c\u306a\u308f\u308c\u305f.\u3053\u306e\u6e2c\u7dda\u306f,\u897f\u5357\u65e5\u672c\u306e\u7279\u5fb4\u7684\u306a\u5730\u8cea\u5e2f\u3092\u5357\u5317\u306b\u6a2a\u5207\u3063\u3066\u3044\u308b.\u7206\u7834\u70b9\u306f\u6e2c\u7dda\u4e0a\u306b\u5168\u90e8\u30676\u30f6\u6240\u8a2d\u3051\u3089\u308c, 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