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  1. H150 博物館
  2. H150b 紀要
  3. 名古屋大学博物館報告
  4. 16

<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.016.04
16dccb81-00c4-4914-9c4a-b87a5fcaca04
名前 / ファイル ライセンス アクション
KJ00000051488.pdf KJ00000051488.pdf (7.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
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

WEKO 4223

ja 萩田, 直子

Search repository
HAGITA, Naoko

× HAGITA, Naoko

WEKO 4224

en HAGITA, Naoko

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足立, 守

× 足立, 守

WEKO 4225

ja 足立, 守

Search repository
ADACHI, Mamoru

× ADACHI, Mamoru

WEKO 4226

en ADACHI, Mamoru

Search repository
志知, 龍一

× 志知, 龍一

WEKO 4227

ja 志知, 龍一

Search repository
SHICHI, Ryuichi

× SHICHI, Ryuichi

WEKO 4228

en SHICHI, Ryuichi

Search repository
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
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
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