著者
三宅 一郎
出版者
同志社大学
雑誌
同志社法學 (ISSN:03877612)
巻号頁・発行日
vol.35, no.5, pp.1-49, 1984-01-31

論説
著者
三宅 一郎
出版者
同志社大学
雑誌
同志社法學 (ISSN:03877612)
巻号頁・発行日
vol.35, no.4, pp.1-58, 1983-11-30

論説
著者
三宅 一郎
出版者
同志社大学
雑誌
同志社法學 (ISSN:03877612)
巻号頁・発行日
vol.35, no.1, pp.1-53, 1983-05-31

論説
著者
三宅 一郎
出版者
同志社大学
雑誌
同志社法學 (ISSN:03877612)
巻号頁・発行日
vol.34, no.5, pp.1-44, 1983-01-31

論説
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

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).
著者
羽鳥 徳太郎
出版者
東京大学地震研究所
雑誌
東京大学地震研究所彙報 (ISSN:00408972)
巻号頁・発行日
vol.54, no.2, pp.343-350, 1979-12-25

The Oshima tsunami of Aug. 29, 1741 (Kampo 1) is the largest tsunami (Imamura-Iida scale m=3) generated in the Japan Sea. According to old documents, the wide area (length 500 km) from west Hokkaido, Tsugaru to Sado Is. suffered severe damage by this tsunami. 1,467 persons were drowned at various villages within 120 km (Matsumae to Kumaishi) along the west coast of the Oshima Peninsula. In the temples of Matsumae and Esashi, there are old monuments which were built just after the tsunami to pray for the repose of the tsunami victims. From the present field investigation, these tsunami monuments are illustrated. Considering ground level, inundation heights of the tsunami along the west coast of the Oshima Peninsula seem to have reached 6 to 8 m with the localized run-up maximum of about 15 meters. The eruptions of the Oshima volcano began 11 days before the tsunami generation and the volcanic activity continued for three months, but earthquakes were not recorded. Judging from the tsunami magnitude and the distribution pattern of wave-heights, it seems that the source area of tsunami extends 100 km or more along a bathymetric line of 3,000 m off the Oshima Peninsula.
著者
阿部 顕治 礒邉 顕生 山根 洋右 小笹 正三郎 吉富 裕之 山田 幸子
出版者
島根大学
雑誌
島根医科大学紀要 (ISSN:03879097)
巻号頁・発行日
vol.14, pp.45-53, 1991-12

Four cases of cutaneous gnathostomiasis successively occurred in 1989 were reported with references to the loaches as the source of infection. The patients complained of migratory cutaneous swellings of their faces or the creeping eruption of the body after they took raw loaches at the Japanese restaurant in Tamayu-cho. They were diagnosed as cutaneous gnathostomiasis by their clinical course and immunological tests. Furthermore, loaches obtained from the Japanese restaurant were investigated, which were imported from China. We suspected Gnathostoma hispidum as the infection source, but no Gnathostoma hispidum were found in loaches except many worms of Nematodes, Pallisentis spp.
著者
Rikitake Tsuneji
出版者
東京大学地震研究所
雑誌
東京大學地震研究所彙報 (ISSN:00408972)
巻号頁・発行日
vol.34, no.4, pp.283-289, 1957-01-30

Magneto-hydrodynamic oscillations of a simple mode are studied in relation to the stability condition of the earth's dynamo. The influence of the Coriolis force is found to be considerable. The previous result, that the toroidal magnetic field would not be large in order to have a stable dynamo, should be abandoned when we take the earth's rotation into account. It seems acceptable that strong magnetic fields which have been suggested by E. C. Bullard exist in the earth's core.
著者
上尾 庄次郎 上田 寛一 山本 義公
出版者
公益社団法人日本薬学会
雑誌
薬学雑誌 (ISSN:00316903)
巻号頁・発行日
vol.86, no.12, pp.1172-1184, 1966-12

The structure of anhydrotaxininol, C_<20>H_<28>O_4,obtained by treatment of taxinine, a constituent of Taxus cuspidata SIEB. et ZUCC., with alcoholic sodium hydroxide, has been briefly reported in a preliminary communication.^<8)> In this paper, details of experimental results and the discussion which led to the assignment of structure III to anhydrotaxininol are presented.