文献一覧: 金子史朗 (著者)

2 0 0 0 OA 大分県中・西部の構造地形と大分県中部地震

著者: 村井勇金子史朗
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 = Bulletin of the Earthquake Research Institute, University of Tokyo (ISSN:00408972)
巻号頁・発行日: vol.50, no.3, pp.329-342, 1976-03-31

2020-07-10 03:23:54
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http://hdl.handle.net/2261/12600

2 0 0 0 OA 桂川谷、四方津ふきんの割れ目地質

著者: 金子史朗
出版者: 一般社団法人日本地質学会
雑誌: 地質学雑誌 (ISSN:00167630)
巻号頁・発行日: vol.65, no.767, pp.470-482, 1959-08-25 (Released:2008-04-11)
参考文献数: 24

2016-06-26 18:48:33
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1 0 0 0 OA 多摩丘陵西辺部と古相模川との関係

著者: 金子史朗
出版者: The Association of Japanese Geographers
雑誌: 地理学評論 (ISSN:00167444)
巻号頁・発行日: vol.31, no.8, pp.495-499, 1958-08-01 (Released:2008-12-24)
参考文献数: 7

The “Gotentoge” gravel bed found on the hill tops of the western part of Tama hills to the south of Hachioji, Tokyo, consists of polygenetic gravels, which seem to have been transported and deposited by the ancient Sagami River, because there exists the lithologic similarity of gravels between the “Gotentoge” gravel bed and the present Sagami River, and also because the gravels of the “Gotentoge” gravel bed become larger as they approach the present Sagami River (Fig. 3). There are some other evidences to prove it. The upper surface of the “Gotentoge” gravel bed is almost horizontal, and covered conformably with the old Kanto volcanic ash member at Terazawa (loc. 4 in Fig. 3), but their stratigraphic relation is almost contemporaneous in the Gotentoge pass. Therefore, the geologic age of the Gotentoge gravel bed is nearly the same with the Kanto volcanic ash member which belongs to the lower Diluvium. Many questions, however, remain unsolved for further study.