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沖縄県石垣島産造礁サンゴ化石の230Th/234U年代とその意義
https://doi.org/10.24517/00063642
https://doi.org/10.24517/0006364275fd2937-2a4b-4534-befc-79162bd62a06
名前 / ファイル | ライセンス | アクション |
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SC-PR-OMURA-A-113_19.pdf (625.8 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-08-30 | |||||
タイトル | ||||||
タイトル | 沖縄県石垣島産造礁サンゴ化石の230Th/234U年代とその意義 | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.24517/00063642 | |||||
ID登録タイプ | JaLC | |||||
著者 |
山田, 茂昭
× 山田, 茂昭× 松田, 博貴× 大村, 明雄 |
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著者別名 |
Yamada, Shigeaki
× Yamada, Shigeaki× Matsuda, Hideaki× Omura, Akio |
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提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学理工研究域自然システム学系 | |||||
書誌情報 |
地質学雑誌 en : The Journal of the Geological Society of Japan 巻 113, 号 1, p. 19-22, 発行日 2007 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0016-7630 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1349-9963 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00141768 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.5575/geosoc.113.19 | |||||
出版者 | ||||||
出版者 | 日本地質学会 The Geological Society of Japan | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This study provides new uranium-series dates of the Ryukyu Group in Ishigaki-jima Island, South Ryukyu Arc (SRA). Two fossil hermatypic coral samples taken from coral limestone in the northern and southern parts of the island were dated as 118.5±2.0 ka and 119.9±2.0 ka, respectively, which correlates to oxygen isotope stage 5.5. This fact suggests that a reef complex was formed during isotope stage 5.5 in Ishigaki-jima Island, just like in Hateruma-jima and Yonaguni-jima Islands, SRA. The dated coral in the northern part was collected at an elevation of 1.3 m. It is, therefore, inferred that the northern part of the island was tectonically stable since isotope stage 5.5. On the other hand, the dated corals in the southern part was collected at an elevation of 15 m, which indicated that the southern part of Ishigaki-jima has been uplifted at rate of about 0.10 m/ky since isotope stage 5.5. Our data clearly show that the western part of SRA has been situated in the tectonic setting of uprift for the last 125 ky. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Uranium-series dates of fossil hermatypic corals in Ishigaki-jima Island, Okinawa Prefecture, and their significance | |||||
権利 | ||||||
権利情報 | Copyright © 日本地質学会 The Geological Society of Japan | |||||
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 | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://www.geosociety.jp | |||||
関連名称 | http://www.geosociety.jp | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/ | |||||
関連名称 | https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/ |