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).
雑誌名
地震研究所研究速報
巻
13
ページ
85 - 126
発行年
1974-03
書誌レコードID
AN10165194
日本十進分類法
051.1
出版者
東京大学地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
1891年濃尾地震の地震断層
jis0130008.pdf
(5.29MB)
