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Tnickness of the Crustal Layer Consisting of Deformed Geosynclinal Sediments
http://hdl.handle.net/10091/10464
http://hdl.handle.net/10091/10464794a5f94-7c8d-4ae0-ab87-48657e9d002b
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
Science07-01-05.pdf (2.8 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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| 公開日 | 2010-10-06 | |||||||
| タイトル | ||||||||
| タイトル | Tnickness of the Crustal Layer Consisting of Deformed Geosynclinal Sediments | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| 資源タイプ | ||||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||||
| タイプ | departmental bulletin paper | |||||||
| 著者 |
YAMASHITA, NOBORU
× YAMASHITA, NOBORU
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| 出版者 | ||||||||
| 出版者 | 信州大学理学部 | |||||||
| 引用 | ||||||||
| 内容記述 | 信州大学理学部紀要 7(1): 29-58(1972) | |||||||
| 書誌情報 |
信州大学理学部紀要 巻 7, 号 1, p. 29-58, 発行日 1972-10-20 |
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| 抄録 | ||||||||
| 内容記述 | The thickness of the crustal layer consisting of deformed geosynclinal sediments is examined, where the Chichibu Palaeozoic Formation, ranging from the middle Silurian to the upper Permian, is taken up as an example. The surface area of each System, though the Silurian and Devonian are combined, is measured on geological maps, and is compared with the stratigraphical thickness. As the surface area and thickness of each System are not in proportion to each other, the overall structure, in spite of the apparent complication, is inferred not to be deep isoclinal folds. The extremely large area of the upper strata compared with the small area of the lower strata indicates a broad and flat syncline including steeper folds of lower order (Fig. 7). The thickness of the crustal layer in question is inferred to be a little larger than, and scarcely attaining two times as large as, the aggregate stratigraphical thickness of the constituent strata. | |||||||
| 資源タイプ（コンテンツの種類） | ||||||||
| ISSN | ||||||||
| 収録物識別子タイプ | PISSN | |||||||
| 収録物識別子 | 0583-063X | |||||||
| 書誌レコードID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA00697923 | |||||||
| 出版タイプ | ||||||||
| 出版タイプ | VoR | |||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||
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Cite as
YAMASHITA, NOBORU, 1972, Tnickness of the Crustal Layer Consisting of Deformed Geosynclinal Sediments: 信州大学理学部, 29–58 p.
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