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Bottom Topography and Sediments in the Area Northwest of Borneo Island
http://hdl.handle.net/10232/13374
http://hdl.handle.net/10232/133747c51ac0f-8498-435b-9a2e-ea8d5ee2fb0c
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 | 2012-05-07 | |||||
タイトル | ||||||
タイトル | Bottom Topography and Sediments in the Area Northwest of Borneo Island | |||||
別言語のタイトル | ||||||
その他のタイトル | ボルネオ島北西海域の海底地形と底質 | |||||
著者 |
HIGASHIKAWA, Seiji
× HIGASHIKAWA, Seiji× UCHIYAMA, Masaki× HIDAKA, Masayasu |
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別言語の著者 | ||||||
姓名 | 東川, 勢二 | |||||
別言語の著者 | ||||||
姓名 | 内山, 正樹 | |||||
別言語の著者 | ||||||
姓名 | 日高, 正康 | |||||
別言語の著者 | ||||||
姓名 | 日髙, 正康 | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Topography | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Sediments | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Median diameter (Md φ) | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Sorting (So) | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Skewness (Sk) | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Bottom current | |||||
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 | |||||
要約(Abstract) | ||||||
内容記述タイプ | Other | |||||
内容記述 | In 1987, T.S.Kagoshima-Maru of the Faculty of Fisheries, Kagoshima University and the University Pertanian Malaysia were engaged in the cooperative survey on the fish resources in the area northwest of Borneo Island. The writers were in charge of surveying bottom topography, sediments and bottom current. The following results were obtained. 1) Continental shelf margin is 175-200m in depth. Continental slope is rather gentle in the western one-thirds of the surveyed area, and rapidly changes into the slope with higher angle eastwards. 2) The bottom sediments of this area are mostly of very fine-grained sands. Their median diameter (Md φ) is ranging from 2.46 to 3.68. 3) Sorting Coefficient (So) ranges from 0.605 to 1.635. This means well-sorted and rather homogeneous sediments. 4) Skewnesses (Sk) of the most samples are plus value, indicating that the grain size composition of the sediments is, as a whole, biassed toward fine grain sizes. 5) Bottom current velocity is generally low, and its direction is unsteady. |
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収録雑誌名 |
鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University 巻 37, p. 111-119 |
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作成日 | ||||||
日付 | 1988-12-25 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
ISSN | 0453087X | |||||
NII書誌ID(雑誌) | ||||||
収録物識別子タイプ | NCID | |||||
NC ID | AN00040498 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
NDC | ||||||
主題Scheme | NDC | |||||
主題 | 452 | |||||
公開者・出版者 | ||||||
出版者 | 鹿児島大学 | |||||
公開者よみ | ||||||
公開者よみ | カゴシマ ダイガク | |||||
公開者別名 | ||||||
公開者別名 | Kagoshima University |