著者

松田 時彦

出版者

東京大学地震研究所

雑誌

地震研究所研究速報

巻号頁・発行日

vol.13, pp.85-126, 1974-03

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The Nobi (Mino-Owari) Earthquake (Table 1) of 1891 is the largest earthquakerecordedi inland in Japan, which was associated with surface faulting of strike-slip type. In this. paper the surface fault localities are reexamined based on Koto (1892), Omori (1894) andi other previous papers and recent field studies. The surface faulting appeard on several pre-existing Quaternary fault line (Figs. 1-3).