WEKO3
アイテム
三波川結晶片岩帯の基本構造について
https://doi.org/10.15027/52527
https://doi.org/10.15027/52527429d3013-dbe8-450e-bc3d-e75aa1a5efdb
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
GeoRepHiroshimaUniv_12_173.pdf (2.1 MB)
|
| Item type | デフォルトアイテムタイプ_（フル）(1) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2023-03-18 | |||||||||
| タイトル | ||||||||||
| タイトル | 三波川結晶片岩帯の基本構造について | |||||||||
| 言語 | ja | |||||||||
| タイトル | ||||||||||
| タイトル | On the Fundamental Structure of the Sambagawa Crystalline Schist Zone | |||||||||
| 言語 | en | |||||||||
| 作成者 |
小島, 丈児
× 小島, 丈児
|
|||||||||
| 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 | |||||||||
| 内容記述 | ||||||||||
| 内容記述 | On the basis of geological and structural data obtained in recent years by the author and his collaborators, the main part of the Sambagawa Crystalline Schist Zone in Shikoku was divided into three structural units with different structural features, namely, 1) the zone of anti-clinorium, 2) the zone of synclinorium, and 3) the zone of flexure between them. The tectonic movement essentially responsible for the formation of the crystalline schist was the downward one located within the zone of synclinorium. Zones of flexure characterized by the features of bedding slide were formed by the movement on the border of the terrain of the downward movement. The terrains outside the zones of flexure, which had not been affected by the movement, were later folded, accompanied with the cleavage of the type of wide spacing. The downward movement was believed to have been set in during the sedimentation of the original geosyncline, probably at the phase of extrusion and intrusion of ophiolitic rocks. | |||||||||
| 言語 | en | |||||||||
| 内容記述 | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | 木野崎吉郎教授退官記念特集号 | |||||||||
| 出版者 | ||||||||||
| 出版者 | 廣島大學理學部地學教室 | |||||||||
| 言語 | ||||||||||
| 言語 | jpn | |||||||||
| 資源タイプ | ||||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||
| 資源タイプ | 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 | 10.15027/52527 | |||||||||
| ID登録タイプ | JaLC | |||||||||
| 収録物識別子 | ||||||||||
| 収録物識別子タイプ | ISSN | |||||||||
| 収録物識別子 | 0073-2303 | |||||||||
| 収録物識別子 | ||||||||||
| 収録物識別子タイプ | NCID | |||||||||
| 収録物識別子 | AN00213676 | |||||||||
| 開始ページ | ||||||||||
| 開始ページ | 173 | |||||||||
| 書誌情報 |
廣島大學地學研究報告 Geological report of the Hiroshima University 号 12, p. 173-182, 発行日 1963-03-30 |
|||||||||
| 旧ID | 52527 | |||||||||
