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東北日本の断裂構造 : とくにグリーン・タフ地域について
https://doi.org/10.15083/00032085
https://doi.org/10.15083/00032085fe1d36ae-872d-45f0-abf9-a30500465903
名前 / ファイル | ライセンス | アクション |
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jis0103001.pdf (991.3 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-12-22 | |||||
タイトル | ||||||
タイトル | 東北日本の断裂構造 : とくにグリーン・タフ地域について | |||||
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 | 10.15083/00032085 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Fracture System developed on the Northeast Japan : Especially on the Green Tuff Region | |||||
著者 |
村井, 勇
× 村井, 勇 |
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著者別名 | ||||||
識別子 | 71255 | |||||
識別子Scheme | WEKO | |||||
姓名 | Murai, Isamu | |||||
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 Japanese Islands are divided into two geological division of Northeast Japan and Southwest Japan by the Itoigawa-Shizuoka Line. The Southwest Japan consists mainly of pre-Neogene rocks and has foundamental framework of structure formed with the pre-Neogene crustal movements, whereas the Northeast Japan is composed predominately of Neogene and Quaternary formations. The major structure of the Northeast Japan is made up by the new tectonic movements which occurred since Miocene epoch centering on the Green Tuff region. The characteristics of geologic structures of the younger formations in the Northeast Japan are built up as the result of interaction between the controlling force of the new tectonic movements and the influcence of old frameworks of the basement structures. They also have intimate interrelationship to the present crustal movements. | |||||
書誌情報 |
地震研究所研究速報 巻 10, 号 3, p. 1-15, 発行日 1973-03 |
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書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN10165194 | |||||
日本十進分類法 | ||||||
主題 | 051.1 | |||||
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 |