37. 福島縣飯坂町近傍の地質に關する二、三の問題に就いて

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In this paper, the writer reports on the results of his geological survey of the Iisaka district, Hukusima Prefecture, north-eastern Japan, in which he concludes that (1) The boundary of the Tertiary strata and the granite that is distributed in the western edge of the Hukusima basin is cut by a fault in both the eastern and western edges of the granite, so that the last-named forms a horst extending north to south. (2) The northern and southern edges of the granite are covered unconformably by Tertiary strata, the basement of which is a talus deposit of granite, the last forming inliers in the Tertiary strata. (3) The geological age and the stratigraphical succession of the Tertiary strata are
東京帝国大学地震研究所,Earthquake Research Institute, Tokyo Imperial University,地震研究所の論文
1943-06-20