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STRATIGRAPHIC CHANGE OF THE COARSE CLASTIC ROCKS OF THE SHIMANTO SUPERGROUP IN EASTERN, SHIKOKU, SOUTHWEST JAPAN
http://hdl.handle.net/10091/12035
http://hdl.handle.net/10091/1203534de0b41-c733-4dfc-833f-77fcbdb20c2e
名前 / ファイル | ライセンス | アクション |
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Item type | 図書 / Book(1) | |||||
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公開日 | 2011-03-16 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | STRATIGRAPHIC CHANGE OF THE COARSE CLASTIC ROCKS OF THE SHIMANTO SUPERGROUP IN EASTERN, SHIKOKU, SOUTHWEST JAPAN | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_2f33 | |||||
タイプ | book | |||||
著者 |
Kumon, Fujio
× Kumon, Fujio |
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信州大学研究者総覧へのリンク | ||||||
氏名 | Kumon, Fujio | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.ZUchOUkh.html | |||||
出版者 | ||||||
出版者 | Terra Scientific Publishing Company | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | Kumon, Fujio. “STRATIGRAPHIC CHANGE OF THE COARSE CLASTIC ROCKS OF THE SHIMANTO SUPERGROUP IN EASTERN, SHIKOKU, SOUTHWEST JAPAN”. Formation of Active Ocean Margins. Nasu, N. Terra Scientific Publishing Company, 1986, p. 819-833. | |||||
書誌情報 |
発行日 1986 |
|||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Shimanto Supergroup of geosynclinal facies which ranges from Cretaceous to early Tertiary in age, is widely distributed in the outermost zone of Southwest Japan. Coeval volcanic and plutonic rocks are extensively distributed in the Inner Zone. The coarse clastic rocks mainly of sandstone occupy about a half of the Shimanto Supergroup, and a stratigraphic change of sandstone and conglomerate composition is recognized in the supergroup. The amount of rock fragments, chiefly acidic to intermediate volcanic rocks, increases upward throughout the Cretaceous sequence. Additionally, acidic tuff layers are frequently intercalated in the Late Cretaceous sequence. Conglomerates in the Late Cretaceous are very dominated by acidic volcanic rock clasts. The geosynclinal sedimentation of the Cretaceous Shimanto Supergroup proceeded with the coeval volcanism which became more active in the Late Cretaceous. The clastic sediments were supplied mainly from the sites of the volcanism. The volcanism corresponds to the Cretaceous volcanic activity in the Inner Zone of Southwest Japan. The Cretaceous Shimanto Supergroup may represent a typical forearc sedimentation in an arc-trench system. | |||||
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 | Book chapter | |||||
ISBN | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | ISBN | |||||
関連識別子 | 9027723028 | |||||
権利 | ||||||
権利情報 | © by Terra Scientific Publishing Company (TERAPUB), Tokyo, 1985. | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |