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岐阜県恵那市に分布する瀬戸層群下部層の古土壌
http://hdl.handle.net/10091/00020561
http://hdl.handle.net/10091/000205611c353859-b522-4a87-9b72-cfe65371ca93
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
Science47-03.pdf (2.2 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||
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| 公開日 | 2018-04-23 | |||||||||||
| タイトル | ||||||||||||
| タイトル | 岐阜県恵那市に分布する瀬戸層群下部層の古土壌 | |||||||||||
| タイトル | ||||||||||||
| タイトル | Paleosols in the lower part of the Seto Group, Ena City, Gifu Prefecture, central Japan | |||||||||||
| 言語 | ||||||||||||
| 言語 | jpn | |||||||||||
| キーワード | ||||||||||||
| 主題 | 瀬戸層群, 中部中新統, 古土壌, 堆積相解析, 粘土鉱物組成 Seto Group, Middle Miocene, paleosol, sedimentary facies analysis, clay mineral assemblage |
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| 資源タイプ | ||||||||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||||||||
| タイプ | departmental bulletin paper | |||||||||||
| 著者 |
葉田野, 希
× 葉田野, 希
× 入江, 志織
× 吉田, 孝
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| 出版者 | ||||||||||||
| 出版者 | 信州大学理学部 | |||||||||||
| 引用 | ||||||||||||
| 内容記述 | Journal of the Faculty of Science Shinshu University 47 : 25-43(2018) | |||||||||||
| 書誌情報 |
Journal of the Faculty of Science Shinshu University 巻 47, p. 25-43, 発行日 2018-03-30 |
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| 抄録 | ||||||||||||
| 内容記述 | The Paleopedological and sedimentological studies were carried out with clay mineralogy on the middle Miocene Tokiguchi Porcelain Clay Formation distributed in Hara Mine in Yamaoka-cho, Ena City, Gifu Prefecture, central Japan. The main part of the Tokiguchi Porcelain Clay Formation,which mainly consists of clay-sized sediments with the alternation of sand and silt sediments,was deposited in stagnant water condition situated in lacustrine environment. The coarse debris flow deposits, however, were predominant in the marginal area of the basin. This wide variety of sedimentary facies is indicative of the diverse and highly undulated morphology. The immature paleosol correlatable to inceptisol, which was intercalated in the debris flow deposits that buried the standing tree trunks,was formed in the marginal area of the sedimentary basin.The mature paleosol correlatable to ultisol was predominant on the emerged lake deposits.These suggest that the whole area of the sedimentary basin was situated by a large fluctuation of the lake water level and ground water table. |
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| 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 | |||||||||||
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| 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 | |||||||||||
