熱ルミネッセンス法による新期雲仙溶岩ドームの年代測定−妙見岳火山以降2万5千年の噴火活動史−
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(3) . ,**- , +- ,**. - - . Thermoluminescence Dating of the Latest Lava Domes at Unzen Volcano, NW Kyushu, Japan Eruption History of the Past ,/,*** Years after Myokendake Volcano Takehiko YAMAGATA, Isao TAKASHIMA, Koichiro WATANABE and Eiji IZAWA Thermoluminescence (TL) ages are obtained for ,2 samples from domes and debris avalanche deposit of Younger Unzen Volcano. Weighted mean ages are ..+*.2 ka for Tenguyama lava, -.2*.0 ka for Shichimenzan lava, -.+*.0 ka for Fugendake-sancho lava, -..*.0 ka for Kazaana lava, +/, ka for Myokendake lava, ,/. ka for Kunimidake lava. Six TL ages for Tarukidaichi debris avalanche deposit range from ,*, ka to -*- ka. We success to distinguish individual dome age by TL dating. Source rock of Tarukidaichi debris avalanche deposit is Kunimidake lava and age range of formation is estimated as ,/ ka to 1.cal ka by TL dating and field observation. We gave new and useful age data of Younger Unzen Volcanic lavas by TL dating with age range about ,/ ka to - ka. Key words : Unzen volcano, thermoluminescence dating, Myoken caldera, devris avalanche deposit, collapsed age. + . bc +33/J K"d ! efge>. ! +33* ++ "#$%&'()*+. XG"hHi1j klm
(4) nm . ,-./0 +330 0 123+4567- 1 8. m1 - op>YX7J. 9:;%<+=*> =?"@+ABC=D%E. _`a1!qrs" ST"t+uvIC. F+G/HIC/J K" 23"LM N"/O"P. YX7+ dw (+331) +x>/yz%{f" N. QNRRG1 ST"UV1WXYGZ [%\. 1W SR S|f"}~g 6. ]+^BC _`aR>Y-ROHCYX7. 7/O1! t"s+-pR!X%XJ. 2+,ῌ2/2+ o 0ῌ+*ῌ+ DD_ ¡¢£ Earth Resources Engineering, Master Course of Graduate School of Engineering, Kyushu University, 0ῌ+*ῌ+, Hakozaki, Higashi-ku, Fukuoka-shi 2+,ῌ 2/2+, Japan. ¤¥¦ : ,0*ῌ*2,0 §d¨oe©ª + «¬®¯ °±¥ Present address : Research Laboratory, Kawatetsu Mining Corporation, +, Niihama-cho, Chuo-ku, Chiba-shi ,0*ῌ*2,0, Japan. *+*ῌ2/*, ²w³´µª +ῌ+ ²wD¶·¸ ¡¹º Research Institute of Materials and Resources, Faculty of Engineering and Resource Science, Akita University, +ῌ+, Tegatagakuen-cho, Akita-shi *+*ῌ. 2/*,, Japan. 2+,ῌ2/2+ o 0ῌ+*ῌ+ DD_ ¡¶ Department of Earth Resources Engineering, Graduate School of Engineering, Kyushu University, 0ῌ+*ῌ+, Hakozaki, Higashi-ku, Fukuoka-shi 2+,ῌ2/2+, Japan. 2+,ῌ2/2+ o 0ῌ+*ῌ+ DD_ ¡ ¶»¼ Professor of Emeritus, Department of Earth Resources Engineering, Graduate School of Engineering, Kyushu University, 0ῌ+*ῌ+, Hakozaki, Higashi-ku, Fukuoka-shi 2+,ῌ2/2+, Japan. Corresponding author : Takehiko Yamagata e-mail : [email protected].
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岸・宮脇(1996)によると,敷地を 含む寺泊・西山丘陵の褶曲運動は約 150万年前以降停止しており,褶曲
敷地からの距離 約82km 火山の形式・タイプ 成層火山.
敷地からの距離 約48km 火山の形式・タイプ 成層火山.