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Foraminiferal evidence of submarine sediment transport and deposition by backwash during the 2004 Indian Ocean tsunami
https://doi.org/10.24517/00029299
https://doi.org/10.24517/00029299311cd912-c926-4df0-a62a-549249964f15
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
RO-PR-TSUKAWAKI-S-513.pdf (533.1 kB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2017-10-05 | |||||
| タイトル | ||||||
| タイトル | Foraminiferal evidence of submarine sediment transport and deposition by backwash during the 2004 Indian Ocean tsunami | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 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 | journal article | |||||
| ID登録 | ||||||
| ID登録 | 10.24517/00029299 | |||||
| ID登録タイプ | JaLC | |||||
| 著者 |
Sugawara, Daisuke
× Sugawara, Daisuke× Minoura, Koji× Nemoto, Naoki× Tsukawaki, Shinji× Goto, Kazuhisa× Imamura, Fumihiko |
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| 著者別表示 |
塚脇, 真二
× 塚脇, 真二 |
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| 書誌情報 |
Island Arc 巻 18, 号 3, p. 513-525, 発行日 2009-01-01 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 1038-4871 | |||||
| NCID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA10848628 | |||||
| DOI | ||||||
| 関連タイプ | isIdenticalTo | |||||
| 識別子タイプ | DOI | |||||
| 関連識別子 | 10.1111/j.1440-1738.2009.00677.x | |||||
| 出版者 | ||||||
| 出版者 | Blackwell Publishing | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Micropaleontological analysis of nearshore to offshore sediments recovered from the southwestern coast of Thailand was performed to clarify the submarine processes of sediment transport and deposition during the 2004 Indian Ocean tsunami. The distribution pattern of benthic foraminifers showed seaward migration after the tsunami event. Agglutinated foraminifers, which are characteristic of an intertidal brackish environment, were identified in the post-tsunami samples from foreshore to offshore zones. These suggest that sediments originally distributed in foreshore to nearshore zones were transported offshore due to the tsunami backwash. On the other hand, the distribution pattern of planktonic and benthic species living in offshore zones showed slight evidence of landward migration by the tsunami. This suggests that landward redistribution of sediments by the tsunami run-up did not occur in the offshore seafloor of the study area. Our results and a review of previous studies provide an interpretation of submarine sedimentation by tsunamis. It is possible that tsunami backwashes induce sediment flows that transport a large amount of coastal materials seaward. Thus, traces of paleotsunami backwashes can be identified in offshore sedimentary environments as the accumulation of allochthonous materials. This can be recognized as changes in benthic foraminiferal assemblages. © 2009 The Authors Journal compilation © 2009 Blackwell Publishing Asia Pty Ltd. | |||||
| 権利 | ||||||
| 権利情報 | © 2009 The Authors Journal compilation © 2009 Blackwell Publishing Asia Pty Ltd.. | |||||
| 著者版フラグ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
