{"_buckets": {"deposit": "0736838c-4d13-4fe9-88b5-f733a665b454"}, "_deposit": {"id": "16137", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "16137"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00016137"}, "item_9_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Studies on Eruptive History of Kuju Volvano : A Review"}]}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2012-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "170", "bibliographicPageStart": "164", "bibliographicVolumeNumber": "23", "bibliographic_titles": [{"bibliographic_title": "\u540d\u53e4\u5c4b\u5927\u5b66\u52a0\u901f\u5668\u8cea\u91cf\u5206\u6790\u8a08\u696d\u7e3e\u5831\u544a\u66f8"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "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). \u4e5d\u91cd\u706b\u5c71\u306f,\u4e5d\u5dde\u4e2d\u90e8\u306e\u963f\u8607\u706b\u5c71\u3068\u7531\u5e03\u5cb3\uff65\u9db4\u898b\u5cb3\u706b\u5c71\u306e\u4e2d\u9593\u306b\u4f4d\u7f6e\u3057,20\u5ea7\u4ee5\u4e0a\u306e\u6eb6\u5ca9\u30c9\u30fc\u30e0\u3084\u5c0f\u578b\u6210\u5c64\u706b\u5c71\u304b\u3089\u306a\u308b\u8907\u6210\u706b\u5c71\u3067\u3042\u308b.Kamata and Kobayashi(1997)\u306f,\u30c6\u30d5\u30e9\u5c64\u5e8f\u306814C\u5e74\u4ee3\u306b\u3082\u3068\u3065\u3044\u3066AT\u4ee5\u964d\u306e\u5674\u706b\u53f2\u3092\u7de8\u3093\u3060\u304c,\u706b\u5c71\u5730\u5f62\u306e\u9bae\u660e\u5ea6\u3084\u5206\u5e03\u95a2\u4fc2\u304b\u3089\u5236\u7d04\u3055\u308c\u308b\u5674\u706b\u9806\u5e8f\u3068\u5408\u81f4\u3057\u306a\u3044\u90e8\u5206\u304c\u3042\u308b.\u7a32\u6c38\u307b\u304b(2006)\u3084\u5965\u91ce\u307b\u304b(2012)\u306eTL\u5e74\u4ee3\u306f,\u76f4\u63a5,\u6eb6\u5ca9\u306e\u5e74\u4ee3\u3092\u793a\u3059\u3053\u3068\u304c\u671f\u5f85\u3067\u304d,\u706b\u5c71\u5730\u5f62\u3068\u3082\u8abf\u548c\u7684\u3067\u3042\u308b.\u5357\u9e93\u306e\u706b\u7815\u6d41\u5806\u7a4d\u7269\u306e14C \u5e74\u4ee3\u3068\u3082\u307b\u307c\u5bfe\u5fdc\u3057,\u5c71\u9802\u4ed8\u8fd1\u306b\u6eb6\u5ca9\u30c9\u30fc\u30e0\u304c\u5f62\u6210\u3055\u308c,\u5c71\u9e93\u306b\u306f\u6eb6\u5ca9\u30c9\u30fc\u30e0\u306e\u5d29\u843d\u306b\u3088\u308b\u706b\u7815\u6d41\u304c\u6d41\u4e0b\u3059\u308b\u3068\u3044\u3046\u30bf\u30a4\u30d7\u306e\u5674\u706b\u3067\u3042\u308b\u3053\u3068\u304c\u308f\u304b\u3063\u3066\u304d\u305f.\u3053\u308c\u3089\u306e\u5674\u706b\u6d3b\u52d5\u304c,\u7d0453kBP\u306e\u98ef\u7530\u706b\u7815\u6d41\u306e\u5674\u51fa\u5f8c.\u3042\u307e\u308a\u9577\u3044\u4f11\u6b62\u671f\u9593\u3092\u7f6e\u304b\u305a\u306b\u30b3\u30f3\u30b9\u30bf\u30f3\u30c8\u306b\u7e70\u308a\u8fd4\u3055\u308c\u305f\u3053\u3068\u304c\u5224\u660e\u3057\u305f.\u3053\u308c\u3089\u306e\u7d50\u679c,\u4e5d\u91cd\u706b\u5c71\u306e\u5674\u51fa\u7387\u306fKamata and Kobayashi(1997)\u306e\u5024\u3088\u308a\u5c0f\u3055\u304f\u306a\u308b\u3068\u8003\u3048\u3089\u308c\u308b.", "subitem_description_type": "Abstract"}]}, 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