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丹後震災地水準測量第1回報告
https://doi.org/10.15083/0000035076
https://doi.org/10.15083/000003507670e58757-e73e-4735-8b70-e7760ce51c7f
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-11-30 | |||||
タイトル | ||||||
タイトル | 丹後震災地水準測量第1回報告 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000035076 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | First Report on the Precise Levelling across the Province of Tango | |||||
著者 |
[著者名なし]
× [著者名なし] |
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著者所属 | ||||||
著者所属 | 地震研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | As stated on p. 163, the Land Survey Department sent us the first report on the precise levelling done along the E-W route which crosses the area where the earthquake was severest and extends to the unaffected districts. The profile of the vertical displacements relative to the height of bench marks measured in 1887 and 1888 is shown in the annexed diagram. A map roughly showing the positions of the faults formed by the earthquake is appended thereto.1) The error of the observation is less than ± 3 mm. in proceeding back and forth over a distance of 2 km.. It is to be understood that at present we are not in a position to fix the line of no displacement, because the western part of the route was more or less disturbed by a strong earthquake which took place in that district two years ago. So that the eastern end where there was apparently no disturbance, was provisionally taken as unaffected and the assumed zero line was drawn on the diagram. | |||||
書誌情報 |
東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University 巻 3, p. 167-169, 発行日 1927-09-20 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00029699 | |||||
日本十進分類法 | ||||||
主題 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
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 |