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糸魚川-静岡構造線の重力調査(III) : 諏訪湖周辺部のブーゲー異常
https://doi.org/10.15083/0000032840
https://doi.org/10.15083/0000032840070123b3-4067-4089-ba04-2478dd591c94
名前 / ファイル | ライセンス | アクション |
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ji0624010.pdf (1.1 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-02-18 | |||||
タイトル | ||||||
タイトル | 糸魚川-静岡構造線の重力調査(III) : 諏訪湖周辺部のブーゲー異常 | |||||
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 | 10.15083/0000032840 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Gravity Observations along the Itoigawa-Shizuoka Geotectonic Line (II) : Bouguer Anomaly in the Suwa Basin, Nagano Prefecture, Central Japan | |||||
著者 |
萩原, 幸男
× 萩原, 幸男× 村田, 一郎× 長沢, 工× 井筒屋, 貞勝× 小竹, 美子× 大久保, 修平× 田島, 廣一 |
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著者別名 | ||||||
識別子 | 127969 | |||||
識別子Scheme | WEKO | |||||
姓名 | Hagiwara, Yukio | |||||
著者別名 | ||||||
識別子 | 127970 | |||||
識別子Scheme | WEKO | |||||
姓名 | Murata, Ichiro | |||||
著者別名 | ||||||
識別子 | 127971 | |||||
識別子Scheme | WEKO | |||||
姓名 | Nagasawa, Ko | |||||
著者別名 | ||||||
識別子 | 127972 | |||||
識別子Scheme | WEKO | |||||
姓名 | Izutuya, Sadakatu | |||||
著者別名 | ||||||
識別子 | 127973 | |||||
識別子Scheme | WEKO | |||||
姓名 | Kotake, Yoshiko | |||||
著者別名 | ||||||
識別子 | 127974 | |||||
識別子Scheme | WEKO | |||||
姓名 | Okubo, Shuhei | |||||
著者別名 | ||||||
識別子 | 127975 | |||||
識別子Scheme | WEKO | |||||
姓名 | Tajima, Hirokazu | |||||
著者所属 | ||||||
著者所属 | 地震研究所 | |||||
著者所属 | ||||||
著者所属 | 日本測量協会 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 諏訪湖周辺に約400点の重力測定を実施した.諏訪湖は糸魚川-静岡構造線の12kmにおよぶ左横ずれ断層運動により生じた陥没地形であって,陥没量は800mを越える.ブーゲー異常から推定すると,陥没量は1~1.4km,横ずれ量は明確ではないが15~20kmと見積ることができる. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Suwa basin is located in the middle part of the Itoigawa-Shizuoka geotectonic line, the left-lateral displacement of which is estimated as about 12 km from geological evidence. The vertical displacement of the basin subsidence amounts to about 800 m. Another important geotectonic line called the Median tectonic line intersects the Itoigawa-Shizuoka line near the Suwa basin. We define gravity field disturbances associated with these faulting activities in considerable detail by concentrating gravity surveying points on the Suwa basin. We clarify gravimetrically the structure around the intersection of the two tectonic lines. Analysis of Bouguer anomaly indicates that the basin subsidence may exceed 1000 m and the lateral offset amounts to 15~20 km, though the latter is not necessarily clear. | |||||
書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 62, 号 4, p. 517-534, 発行日 1988-03-31 |
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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 | AN00162258 | |||||
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 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |