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テフラ編年と14C年代に基づく鹿児島湾奥,新島(燃島)の海成堆積物の編年とその意義
https://doi.org/10.24517/00061618
https://doi.org/10.24517/000616181ab6b661-6b0a-499b-9d32-99bcbcd5c5cd
名前 / ファイル | ライセンス | アクション |
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GS-PR-TANAKA-G-557.pdf (5.6 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-04-15 | |||||
タイトル | ||||||
タイトル | テフラ編年と14C年代に基づく鹿児島湾奥,新島(燃島)の海成堆積物の編年とその意義 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Chronology and Significance of Marine Deposits on Shinjima (Moeshima) Island, Kagoshima Bay, Based on Tephrochronology and 14C Ages | |||||
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 | 10.24517/00061618 | |||||
ID登録タイプ | JaLC | |||||
著者 |
田中, 源吾
× 田中, 源吾× 森脇, 広× 永迫, 俊郎× 西澤, 文勝× 松島, 義章× 鈴木 |
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著者別表示 |
Morikawa, Hiroshi
× Morikawa, Hiroshi× Nagasako, Toshiro× Nishizawa, Fumikatsu× Matsushima, Yoshiaki× Suzuki, Takehiko× Tanaka, Gengo |
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提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学国際基幹教育院GS教育系 | |||||
書誌情報 |
地学雑誌 en : Journal of Geography 巻 126, 号 5, p. 557-579, 発行日 2017-10-25 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0022-135X | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1884-0884 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00322536 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.5026/jgeography.126.557 | |||||
出版者 | ||||||
出版者 | 東京地学協会 Tokyo Geographical Society | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Shinjima (Moeshima) Island in Kagoshima Bay, southern Kyushu, Japan is noteworthy in volcanology, paleontology, and palaeo-environmental studies, because the island emerged from the bay bottom during volcanic activity at Sakurajima in 1780 AD. As a result, Holocene and late-Pleistocene deposits of the bay including muddy deposits, a thick pyroclastic flow deposit, and prominent molluscan shell beds occur on this island. Several tephras included in the bay deposits are critical for deriving their precise chronology. The chronology of those tephras was constructed on the basis of their identification using both refractive indices and major element compositions of constituent glass shards, as well as stratigraphic features in the field. Tephras identified in sediments from younger to older are Sakurajima-Taisho (Sz-Ts)-/P1, Sakurajima-Sueyoshi(Sz-Sy)-/P11, Yonemaru, Sakurajima-Uwaba(Sz-Ub)-/P12, Sakurajima-Takatoge3 (Sz-Tk3)-/P13, Sakurajima-Satsuma (Sz-S)-/P14, and Shinjima pyroclastic flow deposit. The Shinjima pyroclastic flow deposit, which differs stratigraphically between northern and southern areas of Shinjima Island, is the same tephra in the two areas, and is estimated to be c. 13,000 cal BP in age. The pumice clasts of Sz-Sy/P11 provided a suitable environment for the habitat of a prominent shell bed (Moeshima Shell Bed) composed mainly of Neopycnodonte musashiana. Sz-Ub/P12, Sz-Tk3/P13, and associate secondary deposits of Sz-S/P14 indicate that the deposit was formed in the last 13,000 cal BP. The chronology of the deposits of Shinjima Island is based on the findings of stratigraphic positions and ages of those tephras, and 14C ages obtained in this study, and will play an important role when examining the palaeo-environmental history of Kagoshima Bay since the last deglaciation. | |||||
権利 | ||||||
権利情報 | Copyright © 東京地学協会 Tokyo Geographical Society | |||||
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 | https://www.jstage.jst.go.jp/browse/jgeography1889/-char/ja | |||||
関連名称 | https://www.jstage.jst.go.jp/browse/jgeography1889/-char/ja | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://journal.geog.or.jp/ja/ | |||||
関連名称 | http://journal.geog.or.jp/ja/ | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://www.geog.or.jp/ | |||||
関連名称 | http://www.geog.or.jp/ |