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Field logs of Paleogene sediments in Sakito-Oshima and Amakusa-Shimoshima areas, northwestern Kyushu, Southwest Japan
http://hdl.handle.net/10191/2134
http://hdl.handle.net/10191/2134353859a7-9475-44d6-b5ae-47b15acbdfd3
名前 / ファイル | ライセンス | アクション |
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18_53-97.pdf (43.1 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2017-08-24 | |||||
タイトル | ||||||
タイトル | Field logs of Paleogene sediments in Sakito-Oshima and Amakusa-Shimoshima areas, northwestern Kyushu, Southwest Japan | |||||
タイトル | ||||||
タイトル | Field logs of Paleogene sediments in Sakito-Oshima and Amakusa-Shimoshima areas, northwestern Kyushu, Southwest Japan | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Amakusa Coal-Field | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | environment | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | estuary | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | fluvial | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | northwestern Kyushu | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Sakito-Matsushima Coal-Field | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | sedimentary facies | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | shallow marine | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | turbidites | |||||
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 | departmental bulletin paper | |||||
著者 |
Kurita, Hiroshi
× Kurita, Hiroshi× Tateishi, Masaaki× Matsubara, Takashi |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This article reports field observation of Paleogene clastic successions in two areas in north-western Kyushu and provides a preliminary interpretation of their sedimentary environments on the basis of lithological facies. In the sections from Sakito-Oshima Island, the Ichigoshima, Sakito, Maze and Tokuman Formations were logged. They are, except their basal part, interpreted to represent an overall transgression from fluvial, estuarine, shelf, and then to deep marine environments during the latest Eocene to Early Oligocene. A sedimentary cycle of a Middle Eocene age from nonmarine, to deep marine, and then to shallow marine environments was able to be reconstructed from the observation in the sections from the Amakusa-Shimoshima area, where the Fukuregi, Shikiyama and Toishi Formations were examined. These evidence will be adapted in the interpretation of fossil dinoflagellate cysts and molluscs which is the principal intent of the present project. | |||||
書誌情報 |
Science reports of Niigata University. (Geology) en : Science reports of Niigata University. (Geology) 巻 18, p. 53-97, 発行日 2003-03 |
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出版者 | ||||||
出版者 | 新潟大学理学部 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 13491237 | |||||
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収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11436808 | |||||
著者版フラグ | ||||||
値 | publisher |