JpGU-AGU Joint Meeting 2017

講演情報

[JJ] 口頭発表

セッション記号 S (固体地球科学) » S-TT 計測技術・研究手法

[S-TT60] [JJ] ルミネッセンス・ESR測定の年代学・地球惑星科学への貢献

2017年5月24日(水) 15:30 〜 17:00 202 (国際会議場 2F)

コンビーナ:伊藤 一充(産業技術総合研究所地質調査総合センター)、豊田 新(岡山理科大学理学部応用物理学科)、近藤 玲介(皇學館大学教育開発センター)、杉崎 彩子(産業技術総合研究所)、座長:伊藤 一充(産業技術総合研究所地質調査総合センター)、座長:杉崎 彩子(産業技術総合研究所)

16:45 〜 17:00

[STT60-04] ルミネッセンス年代測定による阿蘇火山のカルデラ決壊洪水発生時期の推定

*塚本 すみ子1片岡 香子2宮縁 育夫3 (1.Leibniz Institute for Applied Geophysics、2.新潟大学、3.熊本大学)

キーワード:ルミネッセンス年代測定、post-IR IRSL、テフリックレス、火山性緩傾斜扇状地堆積物

The bouldery volcaniclastic apron sediment (Takuma gravel bed) west of Aso volcano and the overlying tephric loess were studied by Tsukamoto et al (2013) and a preliminary luminescence age constraint of 72-89 ka for the timing of the caldera outburst flood event, which built the volcaniclastic apron, has been reported. In this study we collected additional samples to further constrain the timing of the caldera outburst flood event. Samples were also taken from the Aso-4 ignimbrite, Hotakubo gravel bed consisting of the lower volcaniclasic apron along the Shirakawa River, and the tephric loess deposited above the gravel bed. The luminescence measurements of the tephric loess samples were performed using two post-IR IRSL (pIRIR) protocols with the pIRIR stimulations at 225°C and 290°C. The two pIRIR signals gave consistent ages and the result indicates that the gigantic caldera outburst flood event probably occurred shortly after the Aso-4 eruption, ~86 ka, and the another bouldery Hotakubo gravel bed, which is of cut terrace deposits derived from Takuma gravel bed or of other possible flood event occurred at ~47 ka. The ages will be further compared with the pIRIR ages from the gravel beds themselves. Interestingly, the Aso-4 ignimbrite using the pIRIR signal at 225°C was dated to a much younger age (~40 ka) than the reported eruption age at ~87 ka (Aoki, 2008). This probably indicates that a very long time was needed for the sampled Aso-4 ignimbrite until the temperature reached to the effective closure temperature of the signal (~60-80°C, King et al., 2016).
References
Aoki, K. 2008. Revised age and distribution of ca. 87 ka Aso-4 tephra based on new evidence from the northwest Pacific Ocean. Quaternary International, 178, 100-118.
Tsukamoto, S., Kataoka, K.S., Miyabuchi, Y. 2013. Luminescence dating of volcanogenic outburst flood sediments from Aso volcano and tephric loess deposits, southwest Japan. Geochronometria, 40, 294-303.
King, G.E., Herman, F., Lambert, R., Valla, P.G., Guralnik, B. 2016. Multi-OSL-thermochronometry of feldspar. Quaternary Geochronology, 33, 76-87.