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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 23

九重火山の噴火史研究 (レビュー)

https://doi.org/10.18999/sumrua.23.164
https://doi.org/10.18999/sumrua.23.164
c2b1c408-c4d4-4630-b69f-4834f287038e
名前 / ファイル ライセンス アクション
okuno2011.pdf okuno2011.pdf (6.8 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2013-06-07
タイトル
タイトル 九重火山の噴火史研究 (レビュー)
言語 ja
その他のタイトル
その他のタイトル Studies on Eruptive History of Kuju Volvano : A Review
言語 en
著者 奥野, 充

× 奥野, 充

WEKO 83530

ja 奥野, 充

Search repository
長岡, 信治

× 長岡, 信治

WEKO 83531

ja 長岡, 信治

Search repository
小林, 哲夫

× 小林, 哲夫

WEKO 83532

ja 小林, 哲夫

Search repository
Okuno, Mitsuru

× Okuno, Mitsuru

WEKO 83533

en Okuno, Mitsuru

Search repository
Nagaoka, Shinji

× Nagaoka, Shinji

WEKO 83534

en Nagaoka, Shinji

Search repository
Kobayashi, Tetsuo

× Kobayashi, Tetsuo

WEKO 83535

en Kobayashi, Tetsuo

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
キーワード
主題Scheme Other
主題 九重火山
キーワード
主題Scheme Other
主題 噴火史
キーワード
主題Scheme Other
主題 放射性炭素年代
キーワード
主題Scheme Other
主題 熱ルミネッセンス年代
キーワード
主題Scheme Other
主題 Kuju Volcano
キーワード
主題Scheme Other
主題 Eruptive History
キーワード
主題Scheme Other
主題 Radiocarbon age
キーワード
主題Scheme Other
主題 Thermoluminescence age
抄録
内容記述 We reviewed geological and chronological studies on eruptive history of Kuju volcano, SW Japan. Kuju volcano located between Aso and Yufu-Tsurumi volcanoes in middle Kyushu, consists of lava domes and cones. Although Kamata and Kobayashi (1997) established its eruptive history after AT tephra (30 cal kBP) based on stratigraphic relationships for all eruptive units and 14C ages. However, stratigraphic position of some lava domes was not consistent with their geomorphological features. Recently, the TL ages (Inenaga et al., 2006 and Okuno et al., 2012) expected to indicate the eruptive age of lavas directly are consistent with their volcanic topography. The 14C ages for pyroclastic flow deposits on the south foot (Nagaoka and Okuno, in preparation) can be correlated with TL ages for lavas mentioned above. Therefore, both dating methods will reveal a eruptive sequence (lava dome on mountains and pyroclastic flows on foot). These studies also make clear that these eruptive activities have been repeated after the Handa pyroclastic flows (ca. 53 kBP) without a long dormant period. Therefore, eruptive rate will be smaller than Kamata and Kobayashi (1997).
言語 en
内容記述タイプ Abstract
抄録
内容記述 九重火山は,九州中部の阿蘇火山と由布岳・鶴見岳火山の中間に位置し,20座以上の溶岩ドームや小型成層火山からなる複成火山である.Kamata and Kobayashi(1997)は,テフラ層序と14C年代にもとづいてAT以降の噴火史を編んだが,火山地形の鮮明度や分布関係から制約される噴火順序と合致しない部分がある.稲永ほか(2006)や奥野ほか(2012)のTL年代は,直接,溶岩の年代を示すことが期待でき,火山地形とも調和的である.南麓の火砕流堆積物の14C 年代ともほぼ対応し,山頂付近に溶岩ドームが形成され,山麓には溶岩ドームの崩落による火砕流が流下するというタイプの噴火であることがわかってきた.これらの噴火活動が,約53kBPの飯田火砕流の噴出後.あまり長い休止期間を置かずにコンスタントに繰り返されたことが判明した.これらの結果,九重火山の噴出率はKamata and Kobayashi(1997)の値より小さくなると考えられる.
言語 ja
内容記述タイプ Abstract
内容記述
内容記述 名古屋大学年代測定総合研究センターシンポジウム報告
言語 ja
内容記述タイプ Other
出版者
言語 ja
出版者 名古屋大学年代測定資料研究センター
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.18999/sumrua.23.164
ID登録タイプ JaLC
書誌情報 ja : 名古屋大学加速器質量分析計業績報告書

巻 23, p. 164-170, 発行日 2012-03
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