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<原著論文>重力異常からみた養老断層近傍の地下構造
https://doi.org/10.18999/bulnum.016.04
https://doi.org/10.18999/bulnum.016.0416dccb81-00c4-4914-9c4a-b87a5fcaca04
名前 / ファイル | ライセンス | アクション |
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KJ00000051488.pdf (7.1 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2006-01-06 | |||||
タイトル | ||||||
タイトル | <原著論文>重力異常からみた養老断層近傍の地下構造 | |||||
言語 | ja | |||||
その他のタイトル | ||||||
その他のタイトル | <Original Article>Subsurface structure of the Yoro fault and its environs in central Japan as inferred from gravity anomaly | |||||
言語 | en | |||||
著者 |
萩田, 直子
× 萩田, 直子× HAGITA, Naoko× 足立, 守× ADACHI, Mamoru× 志知, 龍一× SHICHI, Ryuichi |
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アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
抄録 | ||||||
内容記述 | We have newly obtained 2,655 gravity data from a dense gravity survey in an area around the Yoro Mountains, central Japan (Lat. 34°50', Long. 136°25'-136°55'). A new Bouguer anomaly map, drawn from a total of 4,028 gravity data including our new 2,655 data, shows a steep gravity gradient zone of about 10 mgal/km along the eastern slope of the Yoro Mountains. This is one of the steepest gravity gradient zones in the Japanese Islands. The steep gravity gradient zone corresponds to the Yoro fault that forms a clear lineament as the boundary line between the Yoro Mountains and the Nobi Plain. The steep gravity gradient zone does not form a straight line but slightly turns in the middle of the Yoro Mountains. A number of minor faults are observed around the turning point of the steep gravity gradient. We made Bouguer anomaly profiles along the three cross-sections across the Yoro Mountains on the north, middle (the turning point of the steep gravity gradient) and south of them. We inferred the subsurface structure of the Yoro fault by applying the two-dimensional Talwani's method to the profiles. As a result, we estimated the depth of the Yoro fault to be about 2,000 m and the gradient of the fault plane to be over 60°. Comparing the inferred subsurface structures and the geological and topographical features around the Yoro Mountains, we have concluded that the Yoro fault is not one continuous straight fault, but is composed of two faults arranges en echelon. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | 国立情報学研究所で電子化したコンテンツを使用している。 | |||||
言語 | ja | |||||
内容記述タイプ | Other | |||||
出版者 | ||||||
言語 | ja | |||||
出版者 | 名古屋大学博物館 | |||||
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 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
ID登録 | ||||||
ID登録 | 10.18999/bulnum.016.04 | |||||
ID登録タイプ | JaLC | |||||
ISSN(print) | ||||||
収録物識別子タイプ | PISSN | |||||
収録物識別子 | 13468286 | |||||
書誌情報 |
ja : 名古屋大学博物館報告 巻 16, p. 43-89, 発行日 2001-03-21 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/3227 | |||||
識別子タイプ | HDL |