千々石湾茂木沖の海底堆積物の砂粒組成
The shallow water sediments in the north-western part of the Chijiwa Bay off the Mogi coast were analysed by the coarse fraction method which was devised by Shepard and Moore (1954). The average percentage for the constituents in four sediment types which are subdivided into six areal distribution a...
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長崎大学学芸学部
1966
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ftnagasakiuniv:oai:nagasaki-u.repo.nii.ac.jp:00006245 2023-05-15T18:00:55+02:00 千々石湾茂木沖の海底堆積物の砂粒組成 Coarse Fraction Studies of Marine Sediments along the Mogi Coast in Chijiwa Bay, Nagasaki Prefecture 鎌田 泰彦 1966-02-28 http://hdl.handle.net/10069/33171 https://nagasaki-u.repo.nii.ac.jp/?action=repository_uri&item_id=6245 https://nagasaki-u.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6245&item_no=1&attribute_id=18&file_no=1 ja jpn 長崎大学学芸学部 40018180571 https://nagasaki-u.repo.nii.ac.jp/?action=repository_uri&item_id=6245 http://hdl.handle.net/10069/33171 長崎大学学芸学部自然科学研究報告 = Science reports of the Faculty of Arts and Literature, Nagasaki University, 17, 45-54(1966-02-28) 05471419 AN00178087 https://nagasaki-u.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6245&item_no=1&attribute_id=18&file_no=1 長崎大学学芸学部自然科学研究報告. vol.17, p.45-54; 1966 Departmental Bulletin Paper 1966 ftnagasakiuniv 2022-12-02T01:02:00Z The shallow water sediments in the north-western part of the Chijiwa Bay off the Mogi coast were analysed by the coarse fraction method which was devised by Shepard and Moore (1954). The average percentage for the constituents in four sediment types which are subdivided into six areal distribution are illustrated in Figure 3. Type IIa sediments are somewhat poorly sorted sand and are characterized by their preponderant content of terrigenous minerals. Type IIb sediments contain a small amount of silt and clay (15 to 17 per cent of total sample), and a half of the total sample is constituted by terrigenous materials. Shells, Foraminifera and fragments of echinoids are more abundant in silty sand which are classed to Type IIIa, especially in offshore sediments, than the other sediment types. Type III sediments are sandy silt with a dominant amount of silt and clay (65 per cent of total sample) and are characterized by the peculiar organic composition. In this class, the 1/2-1/4 mm size group contain abundant Ostracoda and wood fibers and the 1/8-1/16 mm size group contain many tests of Diatom and planktonic Foraminifera. Report Planktonic foraminifera NAOSITE: Nagasaki University Academic Output SITE |
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Open Polar |
collection |
NAOSITE: Nagasaki University Academic Output SITE |
op_collection_id |
ftnagasakiuniv |
language |
Japanese |
description |
The shallow water sediments in the north-western part of the Chijiwa Bay off the Mogi coast were analysed by the coarse fraction method which was devised by Shepard and Moore (1954). The average percentage for the constituents in four sediment types which are subdivided into six areal distribution are illustrated in Figure 3. Type IIa sediments are somewhat poorly sorted sand and are characterized by their preponderant content of terrigenous minerals. Type IIb sediments contain a small amount of silt and clay (15 to 17 per cent of total sample), and a half of the total sample is constituted by terrigenous materials. Shells, Foraminifera and fragments of echinoids are more abundant in silty sand which are classed to Type IIIa, especially in offshore sediments, than the other sediment types. Type III sediments are sandy silt with a dominant amount of silt and clay (65 per cent of total sample) and are characterized by the peculiar organic composition. In this class, the 1/2-1/4 mm size group contain abundant Ostracoda and wood fibers and the 1/8-1/16 mm size group contain many tests of Diatom and planktonic Foraminifera. |
format |
Report |
author |
鎌田 泰彦 |
spellingShingle |
鎌田 泰彦 千々石湾茂木沖の海底堆積物の砂粒組成 |
author_facet |
鎌田 泰彦 |
author_sort |
鎌田 泰彦 |
title |
千々石湾茂木沖の海底堆積物の砂粒組成 |
title_short |
千々石湾茂木沖の海底堆積物の砂粒組成 |
title_full |
千々石湾茂木沖の海底堆積物の砂粒組成 |
title_fullStr |
千々石湾茂木沖の海底堆積物の砂粒組成 |
title_full_unstemmed |
千々石湾茂木沖の海底堆積物の砂粒組成 |
title_sort |
千々石湾茂木沖の海底堆積物の砂粒組成 |
publisher |
長崎大学学芸学部 |
publishDate |
1966 |
url |
http://hdl.handle.net/10069/33171 https://nagasaki-u.repo.nii.ac.jp/?action=repository_uri&item_id=6245 https://nagasaki-u.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6245&item_no=1&attribute_id=18&file_no=1 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
40018180571 https://nagasaki-u.repo.nii.ac.jp/?action=repository_uri&item_id=6245 http://hdl.handle.net/10069/33171 長崎大学学芸学部自然科学研究報告 = Science reports of the Faculty of Arts and Literature, Nagasaki University, 17, 45-54(1966-02-28) 05471419 AN00178087 https://nagasaki-u.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6245&item_no=1&attribute_id=18&file_no=1 長崎大学学芸学部自然科学研究報告. vol.17, p.45-54; 1966 |
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1766170198856957952 |