{"created":"2023-03-30T09:30:52.454329+00:00","id":3403,"links":{},"metadata":{"_buckets":{"deposit":"4550c43e-6774-46b6-b615-cbe85de3a95e"},"_deposit":{"id":"3403","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"3403"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00003403","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2002-11","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"5","bibliographicPageEnd":"688","bibliographicPageStart":"675","bibliographicVolumeNumber":"47","bibliographic_titles":[{"bibliographic_title":"火山","bibliographic_titleLang":"ja"},{"bibliographic_title":"Bulletin of the Volcanological Society of Japan","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Study on products of phreatomagmatic eruption on 31 March 2000 at Usu volcano gives insight into timing of bubble nucleation and gas escape from system during magma ascent from the reservoir. The essential fragrnents (pumice and micropumice) vary in vesicularity which is negatively correlated to water content in the rhyolitic groundmass glass. This implies that variable vesicularity resulted from different degree of water exsolution from melt to bubbles, rather than different degree of gas escape. The difference in water exsolution probably reflects the different timing of quenching, where ...","subitem_description_language":"ja","subitem_description_type":"Other"},{"subitem_description":"Study on products of phreatomagmatic eruption on 31 March 2000 at Usu volcano gives insight into timing of bubble nucleation and gas escape from system during magma ascent from the reservoir. The essential fragrnents (pumice and micropumice) vary in vesicularity which is negatively correlated to water content in the rhyolitic groundmass glass. This implies that variable vesicularity resulted from different degree of water exsolution from melt to bubbles, rather than different degree of gas escape. The difference in water exsolution probably reflects the different timing of quenching, where ...","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"特定非営利活動法人日本火山学会","subitem_publisher_language":"ja"},{"subitem_publisher":"特定非営利活動法人日本火山学会","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.18940/kazan.47.5_675"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0453-4360","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"鈴木 由希","creatorNameLang":"ja"},{"creatorName":"SUZUKI Yuki","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"中田 節也","creatorNameLang":"ja"},{"creatorName":"NAKADA Setsuya","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_title":"気泡組織・サイズ分布から見た, 有珠山2000年噴火でのマグマ上昇と発泡プロセス(<特集>2000年有珠山噴火 (3))","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"気泡組織・サイズ分布から見た, 有珠山2000年噴火でのマグマ上昇と発泡プロセス(<特集>2000年有珠山噴火 (3))","subitem_title_language":"ja"},{"subitem_title":"Vesiculation and Magma Ascent Process in the Usu 2000 Eruption, Inferred from Texture and Size Distribution of Bubbles(<Special Section>The 2000 Eruption of Usu Volcano (3))","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-03-30"},"publish_date":"2023-03-30","publish_status":"0","recid":"3403","relation_version_is_last":true,"title":["気泡組織・サイズ分布から見た, 有珠山2000年噴火でのマグマ上昇と発泡プロセス(<特集>2000年有珠山噴火 (3))"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-08T01:37:29.366653+00:00"}