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美濃帯根尾―和泉地域の左門岳ユニットから産出したトリアス紀およびジュラ紀の放散虫化石群集
http://hdl.handle.net/10091/10654
http://hdl.handle.net/10091/106549b5b1c99-e8db-4302-a925-93835f84de35
名前 / ファイル | ライセンス | アクション |
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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 | ||||||
言語 | ja | |||||
タイトル | 美濃帯根尾―和泉地域の左門岳ユニットから産出したトリアス紀およびジュラ紀の放散虫化石群集 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Trlassic and Jurassic radiolarian assemblages from the Samondake Unit of the Mino Terrane in the Neo-Izumi area, central Japan | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | radiolarians | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Jurassic | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Samondake Unit | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Mino Terrane | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | melange | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | subduction comple | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
著者 |
小林, 祐哉
× 小林, 祐哉 |
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出版者 | ||||||
出版者 | 信州大学理学部 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 信州大学理学部紀要 33(1): 27-63(1998) | |||||
書誌情報 |
信州大学理学部紀要 巻 33, 号 1, p. 27-63, 発行日 1998-10-30 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Samondake Unit of the Mino Terrane in central Japan is characterized by a large quantity of sandstone. The Samondake Unit in the Neo-Izumi area is divided into the Subunit A and Subunit B on the basis of features in lithology, structure and deformation. The Subunit A is situated structurally higher than the Subunit B, and they are in fault contact each other. Radiolarian age of the Samondake Unit ranges from Middle Triassic to middle Middle Jurassic time. However middle Middle Jurassic radiolarians which characterize the Tricolocapsa plicarum zone (Matsuoka, 1995) are obtained from siliceous mudstone and mudstone of both Subunit A and B, early Middle Jurassic radiolarians which characterize the Laxtorum(?) jurassicum zone are obtained from only some siliceous mudstone of the Subunit A. Both Subunit A and B are considered to have been formed in the subduction accretion process on the basis of the ages and structural relationship of the two units. | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
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 |