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19. 靜岡縣熱海温泉と地質構造との關係一考察
https://doi.org/10.15083/0000034340
https://doi.org/10.15083/00000343407052ebe1-af2b-48bb-a8b8-1404a4448646
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ji0213008.pdf (1.7 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-06-06 | |||||
| タイトル | ||||||
| タイトル | 19. 靜岡縣熱海温泉と地質構造との關係一考察 | |||||
| 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 | 10.15083/0000034340 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | 19. Geologic Consideration of the Abnormal Temperature Distribution in the Hot Springs at Atami, Sizugka Prefecture, Japan | |||||
| 著者 |
大塚, 彌之助
× 大塚, 彌之助 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133466 | |||||
| 姓名 | Otuka, Yanosuke | |||||
| 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 | The writer here briefly describes the relation between the geologic structure and the temperature of the hot springs at Atami, in studying which he has reached the following conclusions: 1. The basal complex of the Atami region consists of Neogene andestic tuffite which are blocked by numerous faults, most of them trending NW-SE. 2. It is from these Neogene tuffites that the heated mineral water at this resort mostly originates. 3. The presence of an underground hot mineral water surface, like an ordinary underground water surface, is inferred. 4, This hot underground mineral water: surface shows characters similar to the ordinary underground water surface. 5. As to the temperature distribution of the mineral water, there is a high temperature section, situated en the northern side or the river Hatu. Geologically speaking, it is bounded by a large, fault, trending NW-SE along the valley of Hatu, and dipping steeply northeastward from Kinomiya to Atami-Ginza. On the northern side of this fault, the Neogene tuffites and lavas have decomposed and metamorphosed into solfataric clay, while on the southern side we find exposed a fresh, side, undecomposed tuffite. The former may have decomposed and metamorphosed into solfataric clay and other soluble materials from the effects of heated gases and hydrothermal solutions during the later stage of activity of the Pleistocene volcano of Taga. 6. Some of the highly heated mineral water is probably ordinary underground water heated by the gases and through hydrothermal solution white the others may be juvenile water derived from these gases and from solutions, particularly those that ascend through the faults and the solfataric clay zone. 7. From the tectonic view point, it may not be easy to rejuvenate the famous ""geyser Ooyu"", at Atami, by merely increasing the depth of the boring, without invoking certain other mechanical aids. | |||||
| 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 21, 号 3-4, p. 414-434, 発行日 1944-08-15 |
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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 | |||||
| フォーマット | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | application/pdf | |||||
| 日本十進分類法 | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 453 | |||||
| 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 | ||||||
