@article{oai:tokyo-metro-u.repo.nii.ac.jp:00005534,
 author = {Matsuda, Iware and 松田, 磐余},
 issue = {57},
 journal = {総合都市研究},
 month = {},
 note = {1995年兵庫県南部地震の被害状況を現地調査した結果を述べた。淡路島内の建物被害の特徴は、地震断層の出現は断層の直上を除けば被害とは密接に関連せず、地盤の影響が強く反映されていることであった。神戸側に震災の帯が出現した理由と地震断層についての調査結果を紹介し、それに筆者らの調査結果を付け加えた。顕著な被害が直線的に配列することは、地震断層そのものの直接的影響とは断定できないが、震源断層に雁行するいくつもの断層もしくは亀裂が地盤の変位をともなう被害を発現させたためであると解釈した。さらに、地形と被害との関係の概要を述べた。, The Hanshin District lies between the Takatsuki-Arima Tectonic Line and Median Tectonic Line. Many active faults called the Rokkou-Awajishima Fault System connect them. The Fault System caused the 1995 Hyogo-ken Nanbu Earthquake. Though a typical earthquake fault appeared along the Nojima Fault in Awajishima，most of damages were due to site effects. The heavily damaged zone appeared in the Kobe and Ashiya Cities. Geological and Geomorphological conditions，a hidden active fault under the recent deposits，movement of the southern extension of active faults lying in the Rokko Mountains，reflection of seismic waves from the basal rock and existence of old buildings are pointed out for the reasons of appearence of the heavily damaged zone. The main cause has not been made clear，but the heavily damaged zone might have been resulted from complex effects of these reasons., postprint},
 pages = {5--18},
 title = {1995年兵庫県南部地震の地震断層と地形から見た被害状況},
 year = {1995}
}