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このアイテムのファイル:
| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| a27b1p13.pdf | 420.54 kB | Adobe PDF | 見る/開く |
| タイトル: | 丹後半島地方の地震活動 (第1報) |
| その他のタイトル: | ON THE SEISMIC ACTIVITY OF TANGO PENINSULA REGION (PART 1) |
| 著者: | 渡辺, 邦彦  見野, 和夫 西田, 良平 松尾, 成光 中尾, 節郎 榎本, 晋 |
| 著者名の別形: | WATANABE, Kunihiko MINO, Kazuo NISHIDA, Ryohei MATSUO, Shigemitsu NAKAO, Setsuro ENOMOTO, Susumu |
| 発行日: | 1-Apr-1984 |
| 出版者: | 京都大学防災研究所 |
| 誌名: | 京都大学防災研究所年報. B |
| 巻: | 27 |
| 号: | B-1 |
| 開始ページ: | 117 |
| 終了ページ: | 124 |
| 抄録: | On March, 1927, Tango Earthquake (M 7.5) occurred at Tango peninsula region, northernpart of Kyoto Pref. And caused much damage to all that neighborhood. Two major fault systems, Gomura echelon fault system and Yamada fault, which were perpendicular with each other movedat this earthquake. So, we settled a seismic observation network with three stations in Tangoregion and have investigated the seismic activity near around this region.The high seismicity near the root area of Tango peninsula and along the Japan-Sea shore isremarkable. The fault plane solutions of four moderate earthquakes were analyzed. Three ofthese were strike-slip type with principal stress axis of ES-NW direction, but the direction of oneother earthquake was perpendicular to those of another three events. |
| URI: | http://hdl.handle.net/2433/70653 |
| 関連リンク: | http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html |
| 出現コレクション: | No.27 B-1 |
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