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To re-examine the eruptive history of the volcano, we performed thermoluminescence (TL) dating for 9 samples from lavas and a lithic fragment of an ignimbrite samples. The obtained ages are 4.9\u00b10.5 ka and 5.7\u00b10.9 ka (weighted mean: 5.1\u00b10.4 ka) for Taisen-minami lava, 22.3\u00b16.2 ka for the summit lava dome of Kujusan, 68.0\u00b13.1 ka for the main edifice of Kujusan, 75.6\u00b17.0 ka for Ogigahana lava, 60.8\u00b16.4 ka for Kutsukakeyama lava, 52.8\u00b13.8 ka for Hosshozan lava, 25.8\u00b11.6 ka for Hizengajo lava and 72.8\u00b15.1 ka for a lithic fragment in the Handa ignimbrite. The 52 ka eruption age obtained for the Handa ignimbrite is estimated from the stratigraphic position between Aso-4 and Aira Tn ash. These TL ages suggest that the Ogigahana lava and the main edifice of Kujusan were formed before the Handa ignimbrite eruption (52 ka), and that immediately before/after the Handa ignimbrite eruption, Kutsukakeyama lava and Hosshozan lava were effused. Furthermore, the Hizengajo lava and the summit lava dome of Kujusan were formed near the summit of the volcano probably after the deposition of Aira Tn ash in 29 ka.", "subitem_description_type": "Abstract"}]}, "item_9_description_5": {"attribute_name": "\u5185\u5bb9\u8a18\u8ff0", "attribute_value_mlt": [{"subitem_description": "\u7b2c18\u56de\u540d\u53e4\u5c4b\u5927\u5b66\u5e74\u4ee3\u6e2c\u5b9a\u7dcf\u5408\u7814\u7a76\u30bb\u30f3\u30bf\u30fc\u30b7\u30f3\u30dd\u30b8\u30a6\u30e0\u5e73\u621017(2005)\u5e74\u5ea6\u5831\u544a Proceedings of the 18th symposiumon on Chronological Studies at the Nagoya University Center for Chronological Research\\\nin 2005 \u65e5\u6642:\u5e73\u621018 (2006)\u5e741\u670817\u65e5(\u706b)\uff6418\u65e5(\u6c34) \u4f1a\u5834:\u540d\u53e4\u5c4b\u5927\u5b66\u30b7\u30f3\u30dd\u30b8\u30aa\u30f3 Date:Januaryl7th and 18th, 2006 Venue:Nagoya Uhiversity Symposion Hall", "subitem_description_type": "Other"}]}, "item_9_identifier_registration": {"attribute_name": 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