地形から地殻の移動從て地殻に働く歪力を判断することの可能度に就いて

地形から地殻の移動從て地殻に働く歪力を判断することの可能度に就いて利用統計を見る

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アイテムタイプ	紀要論文 / Departmental Bulletin Paper
言語	日本語
その他のタイトル	On the Possibility of Finding Stresses acting on and Displacements of the Earthcrust from its surface form
著者	藤原咲平高山威雄
著者別名	Fujiwhara S. Takayama T.
著者所属	地震研究所
抄録	The authors formerly established the law governing the relation between the sense of rotation or shear and that of produced vortex or echelon crack in connection with the divergence or convergence. They already applied the law to the analysis of the Great Japanese Earthquake on Sept. 1, 1923, and found the close agreement of the law with facts. In the present note they point out that the law is quite fulfilled by the echelon cracks of G6-mura fault produced on the occasion of Tango-Earthquake on March 7, 1927. In virtue, of the present law the sence of the echelon suggests to us the existence of compressive and anticlockwise shear along the fault, and the recent actual surveying of the district by the Land Survey Department of Japan proved that this is just the case.
雑誌名	東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University
巻	7
号	3
ページ	523 - 530
発行年	1930-04-08
ISSN	00408972
書誌レコードID	AN00029699
フォーマット	application/pdf
日本十進分類法	453
出版者	東京帝国大学地震研究所
出版者別名	Earthquake Research Institute, Tokyo Imperial University