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IODP Expedition 317: Exploring the Record of Sea-Level Change Off New Zealand
http://hdl.handle.net/10091/00019020
http://hdl.handle.net/10091/000190200f1b99bf-0920-44cc-9dfc-acbae8845e73
| 名前 / ファイル | ライセンス | アクション |
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Exploring_the_Record_of_Sea-Level_Change_Off_New_Zealand.pdf (1.6 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
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| 公開日 | 2016-08-19 | |||||
| タイトル | ||||||
| タイトル | IODP Expedition 317: Exploring the Record of Sea-Level Change Off New Zealand | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| DOI | ||||||
| 識別子タイプ | DOI | |||||
| 関連識別子 | https://doi.org/10.2204/iodp.sd.12.01.2011 | |||||
| 関連名称 | 10.2204/iodp.sd.12.01.2011 | |||||
| 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 | |||||
| 著者 |
Fulthorpe, CS
× Fulthorpe, CS× Hoyanagi, K× Blum, P× IODP, Expedition 317 Scientists, |
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| 信州大学研究者総覧へのリンク | ||||||
| 表示名 | Hoyanagi, Koichi | |||||
| URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.jpDmOUkh.html | |||||
| 出版者 | ||||||
| 出版者 | Copernicus Publications | |||||
| 引用 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Scientific Drilling. 12:4-14 (2011) | |||||
| 書誌情報 |
Scientific Drilling 巻 12, p. 4-14, 発行日 2012 |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Expedition 317 investigated the record of global sea-level change (eustasy) within continental margin sedimentary to produce preserved sedimentary architectures. The Canterbury Basin, on the eastern margin of the South Island because of high rates of Neogene sediment supply from the uplifting Southern Alps. This sediment input results in a high-frequency (~0.1–0.5 My periods) record of depositional cyclicity that is modulated by the presence of strong ocean currents. The expedition recovered sediments as old as Eocene but focused on the sequence stratigraphy of the late Miocene to Recent, when global sea-level change was dominated by glacioeustasy. A transect of three sites was drilled on the continental shelf (Sites U1353, U1354, and U1351), plus one on the continental slope (Site U1352). The transect samples the shallow-water environment most directly affected by relative sea-level change. Lithologic boundaries, provisionally correlative with seismic sequence boundaries, have been identified in cores from each site. Continental slope Site U1352 provides a record of ocean circulation and fronts during the last ~35 My. The early Oligocene (~30 Ma) Marshall Paraconformity was the deepest target of Expedition 317 and is hypothesized to represent intensified current erosion or non-deposition associated with the initiation of thermohaline circulation in the region. Expedition 317 involved operational challenges for JOIDES Resolution, including shallow-water, continental-shelf drilling and deep penetrations. Despite these challenges, Expedition 317 set a number of records for scientific ocean drilling penetration and water-depth. | |||||
| 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 | Article | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 1816-8957 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA12314103 | |||||
| 権利 | ||||||
| 権利情報 | © 2011 Author(s). This work is distributedunder the Creative Commons Attribution 3.0 License. | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
