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九州四万十帯，古第三系日向層群のデュープレックス構造と赤・緑色珪質泥岩
https://tokushima-u.repo.nii.ac.jp/records/2010463
https://tokushima-u.repo.nii.ac.jp/records/2010463239ccd59-eb57-4854-88bc-9b884beef205
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
trgj_40_21.pdf (2.75 MB)
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| Item type | 文献 / Documents(1) | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2022-11-10 | |||||||||||
| アクセス権 | ||||||||||||
| アクセス権 | open access | |||||||||||
| 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 | journal article | |||||||||||
| 出版社版DOI | ||||||||||||
| 関連識別子 | http://struct.geosociety.jp/pub/trgj/40/4003.pdf | |||||||||||
| 出版タイプ | ||||||||||||
| 出版タイプ | VoR | |||||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||
| タイトル | ||||||||||||
| タイトル | 九州四万十帯，古第三系日向層群のデュープレックス構造と赤・緑色珪質泥岩 | |||||||||||
| タイトル別表記 | ||||||||||||
| その他のタイトル | Duplex structures and red & green siliceous mudstones of the Paleogene Hyuga Group in the Shimanto Terrane, Kyushu, Southwest Japan | |||||||||||
| タイトル別表記 | ||||||||||||
| その他のタイトル | 日向層群のデュープレックス | |||||||||||
| 著者 |
村田, 明広
× 村田, 明広
WEKO
157
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| 抄録 | ||||||||||||
| 内容記述 | The Paleogene Hyuga Group of the NE Miyakonojo and Aradani Areas in Kyushu consists of sandstone-dominated formation, mudstone-dominated formation, and chaotic formation. They are altemately repeated by originally low-angled thrusts, and probably form duplex structures. The duplexes of the Hyuga Group are in most cases hinterland-dipping duplex. The fundamental structure of the Paleogene Shimanto Terrane in Kyushu is characterized by low-angled nappe structures with stacked duplexes, in which duplexes lie one above the other, similarly to those of the Cretaceous Uchinohae Formation. Red and green siliceous mudstones of Middle Eocene age occur along major thrusts as thrust sheets of 40 to 80 m thick. The siliceous mudstones, which are considered to be hemipelagic sediments, were subducted, and formed thrust sheets during underplating. The siliceous mudstones were probably situated in the decollement horizons, but were not flowed as a lubricant layer. | |||||||||||
| 書誌情報 |
ja : 構造地質 巻 40, p. 21-29, 発行日 1994-09 |
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| 収録物ID | ||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||
| 収録物識別子 | AA11457546 | |||||||||||
| 出版者 | ||||||||||||
| 出版者 | 日本地質学会構造地質研究会 | |||||||||||
| EID | ||||||||||||
| 識別子 | 61201 | |||||||||||
| 言語 | ||||||||||||
| 言語 | jpn | |||||||||||
