WEKO3
アイテム
{"_buckets": {"deposit": "d97f7046-f9e7-4226-a6d0-ca403f23a28d"}, "_deposit": {"created_by": 1, "id": "29870", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "29870"}, "status": "published"}, "_oai": {"id": "oai:kumadai.repo.nii.ac.jp:00029870", "sets": ["444"]}, "author_link": ["137535", "137542", "137543", "147383", "137537", "137536"], "item_16_alternative_title_22": {"attribute_name": "その他の言語のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "Rhyolite to Dacite Lava Flows Newly-discovered on the Western Slope of Aso Central Cones, Southwestern Japan"}]}, "item_16_alternative_title_23": {"attribute_name": "タイトル(ヨミ)", "attribute_value_mlt": [{"subitem_alternative_title": "アソ チュウオウ カコウ キュウグン ニシガワ シャメン ニ オイテ アラタニ ハッケン サレタ リュウモンガン : デイサイトシツ ヨウガンリュウ"}]}, "item_16_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2004-06-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "3", "bibliographicPageEnd": "128", "bibliographicPageStart": "119", "bibliographicVolumeNumber": "49", "bibliographic_titles": [{"bibliographic_title": "火山"}]}]}, "item_16_creator_3": {"attribute_name": "別言語の著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorAffiliations": [{"affiliationNameIdentifiers": [{"affiliationNameIdentifier": "", "affiliationNameIdentifierScheme": "ISNI", "affiliationNameIdentifierURI": "http://www.isni.org/isni/"}], "affiliationNames": [{"affiliationName": "", "affiliationNameLang": "ja"}]}], "creatorNames": [{"creatorName": "増田, 直朗", "creatorNameLang": "ja"}, {"creatorName": "マスダ, ナオアキ", "creatorNameLang": "ja-Kana"}, {"creatorName": "Masuda, Naoaki", "creatorNameLang": "en"}], "familyNames": [{"familyName": "増田", "familyNameLang": "ja"}, {"familyName": "マスダ", "familyNameLang": "ja-Kana"}, {"familyName": "Masuda", "familyNameLang": "en"}], "givenNames": [{"givenName": "直朗", "givenNameLang": "ja"}, {"givenName": "ナオアキ", "givenNameLang": "ja-Kana"}, {"givenName": "Naoaki", "givenNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "147383", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Watanabe, Kazunori"}], "nameIdentifiers": [{"nameIdentifier": "137542", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Miyabuchi, Yasuo"}], "nameIdentifiers": [{"nameIdentifier": "137543", "nameIdentifierScheme": "WEKO"}]}]}, "item_16_description_17": {"attribute_name": "フォーマット", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_16_description_46": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"subitem_description": "論文(Article)", "subitem_description_type": "Other"}]}, "item_16_description_5": {"attribute_name": "内容記述", "attribute_value_mlt": [{"subitem_description": "Three lava flows: Nakahono, Nagano, Otogase lava flows and Otogase debris avalanche deposit were newly discovered on the western slope of Aso central cones, southwestern Japan. The Nakahono lava is biotite rhyolite (SiO2=73 wt.%) and is distributed on only a floor of the Otogasegawa River. Occurrence age of the Nakahono lava is older than that of ACP3 or ACP5. The Nagano lava is pyroxene dacite (SiO2=68 wt.%) and comprises a pyroclastic cone (ca. 600 m diameter). The Otogase lava is pyroxene rhyolite (SiO2=73 wt.%) and forms a lava plateau (ca. 1 km long and 200-300 m wide). The lava is intervedded between the Aira-Tn ash (AT, ca. 29 cal ka) and the Kikai Akahoya ash (K-Ah, ca. 7.3 cal ka). The Otogase debris avalanche deposit is possibly generated by a collapse of lava flow or dome on the vent of the Otogase lava. Based on the stratigraphic relationship with tephra deposits, the eruption age was estimated at ca. 20 cal ka. In the period of younger stage than approximately 30 cal ka, intermittent eruptions producing three rhyolite to dacite lava flows provide important information about eruptive history and magma evolution in the western part of Aso central cones.", "subitem_description_type": "Other"}]}, "item_16_description_77": {"attribute_name": "URL", "attribute_value_mlt": [{"subitem_description": "https://www.jstage.jst.go.jp/article/kazan/49/3/49_KJ00002524747/_article/-char/ja/", "subitem_description_type": "Other"}]}, "item_16_publisher_36": {"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"}]}, "item_16_relation_11": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type": "isIdenticalTo", "subitem_relation_type_id": {"subitem_relation_type_id_text": "http://doi.org/10.18940/kazan.49.3_119", "subitem_relation_type_select": "DOI"}}]}, "item_16_rights_12": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "© 2004 特定非営利活動法人日本火山学会"}]}, "item_16_source_id_7": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "04534360", "subitem_source_identifier_type": "ISSN"}]}, "item_16_source_id_9": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN10512786", "subitem_source_identifier_type": "NCID"}]}, "item_16_subject_20": {"attribute_name": "日本十進分類法", "attribute_value_mlt": [{"subitem_subject": "453.8", "subitem_subject_scheme": "NDC"}]}, "item_16_text_18": {"attribute_name": "形態", "attribute_value_mlt": [{"subitem_text_value": "5598446 bytes"}]}, "item_16_text_47": {"attribute_name": "資源タイプ・ローカル", "attribute_value_mlt": [{"subitem_text_value": "雑誌掲載論文"}]}, "item_16_text_48": {"attribute_name": "資源タイプ・NII", "attribute_value_mlt": [{"subitem_text_value": "Journal Article"}]}, "item_16_text_49": {"attribute_name": "資源タイプ・DCMI", "attribute_value_mlt": [{"subitem_text_value": "text"}]}, "item_16_text_50": {"attribute_name": "資源タイプ・ローカル表示コード", "attribute_value_mlt": [{"subitem_text_value": "01"}]}, "item_16_text_76": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_text_value": "http://hdl.handle.net/2298/36983"}]}, "item_16_version_type_19": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "増田, 直朗"}], "nameIdentifiers": [{"nameIdentifier": "137535", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "渡辺, 一徳"}], "nameIdentifiers": [{"nameIdentifier": "137536", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "宮縁, 育夫"}], "nameIdentifiers": [{"nameIdentifier": "137537", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2020-03-03"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "kazan49(3)_119-128.pdf", "filesize": [{"value": "5.6 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 5600000.0, "url": {"label": "kazan49(3)_119-128.pdf", "url": "https://kumadai.repo.nii.ac.jp/record/29870/files/kazan49(3)_119-128.pdf"}, "version_id": "4511572c-8f79-4cc3-8213-56968120dbe8"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "lava", "subitem_subject_scheme": "Other"}, {"subitem_subject": "ryolite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "dacite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "debris avalanche", "subitem_subject_scheme": "Other"}, {"subitem_subject": "tephra", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "jpn"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "阿蘇中央火口丘群西側斜面において新たに発見された流紋岩 : デイサイト質溶岩流", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "阿蘇中央火口丘群西側斜面において新たに発見された流紋岩 : デイサイト質溶岩流"}]}, "item_type_id": "16", "owner": "1", "path": ["444"], "permalink_uri": "http://hdl.handle.net/2298/36983", "pubdate": {"attribute_name": "公開日", "attribute_value": "2017-05-10"}, "publish_date": "2017-05-10", "publish_status": "0", "recid": "29870", "relation": {}, "relation_version_is_last": true, "title": ["阿蘇中央火口丘群西側斜面において新たに発見された流紋岩 : デイサイト質溶岩流"], "weko_shared_id": -1}
阿蘇中央火口丘群西側斜面において新たに発見された流紋岩 : デイサイト質溶岩流
http://hdl.handle.net/2298/36983
http://hdl.handle.net/2298/36983ff80ebe8-265f-49e7-b710-27900ce3c2e3
名前 / ファイル | ライセンス | アクション |
---|---|---|
kazan49(3)_119-128.pdf (5.6 MB)
|
|
Item type | 学術雑誌論文 / Journal Article(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2017-05-10 | |||||
タイトル | ||||||
タイトル | 阿蘇中央火口丘群西側斜面において新たに発見された流紋岩 : デイサイト質溶岩流 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | lava, ryolite, dacite, debris avalanche, tephra | |||||
資源タイプ | ||||||
資源タイプ | journal article | |||||
著者 |
増田, 直朗
× 増田, 直朗× 渡辺, 一徳× 宮縁, 育夫 |
|||||
別言語の著者 |
増田, 直朗
× 増田, 直朗× Watanabe, Kazunori× Miyabuchi, Yasuo |
|||||
内容記述 | ||||||
内容記述 | Three lava flows: Nakahono, Nagano, Otogase lava flows and Otogase debris avalanche deposit were newly discovered on the western slope of Aso central cones, southwestern Japan. The Nakahono lava is biotite rhyolite (SiO2=73 wt.%) and is distributed on only a floor of the Otogasegawa River. Occurrence age of the Nakahono lava is older than that of ACP3 or ACP5. The Nagano lava is pyroxene dacite (SiO2=68 wt.%) and comprises a pyroclastic cone (ca. 600 m diameter). The Otogase lava is pyroxene rhyolite (SiO2=73 wt.%) and forms a lava plateau (ca. 1 km long and 200-300 m wide). The lava is intervedded between the Aira-Tn ash (AT, ca. 29 cal ka) and the Kikai Akahoya ash (K-Ah, ca. 7.3 cal ka). The Otogase debris avalanche deposit is possibly generated by a collapse of lava flow or dome on the vent of the Otogase lava. Based on the stratigraphic relationship with tephra deposits, the eruption age was estimated at ca. 20 cal ka. In the period of younger stage than approximately 30 cal ka, intermittent eruptions producing three rhyolite to dacite lava flows provide important information about eruptive history and magma evolution in the western part of Aso central cones. | |||||
書誌情報 |
火山 巻 49, 号 3, p. 119-128, 発行年 2004-06-30 |
|||||
ISSN | ||||||
収録物識別子 | 04534360 | |||||
書誌レコードID | ||||||
収録物識別子 | AN10512786 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
関連識別子 | http://doi.org/10.18940/kazan.49.3_119 | |||||
権利 | ||||||
権利情報 | © 2004 特定非営利活動法人日本火山学会 | |||||
フォーマット | ||||||
内容記述 | application/pdf | |||||
形態 | ||||||
5598446 bytes | ||||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
日本十進分類法 | ||||||
主題 | 453.8 | |||||
その他の言語のタイトル | ||||||
その他のタイトル | Rhyolite to Dacite Lava Flows Newly-discovered on the Western Slope of Aso Central Cones, Southwestern Japan | |||||
タイトル(ヨミ) | ||||||
その他のタイトル | アソ チュウオウ カコウ キュウグン ニシガワ シャメン ニ オイテ アラタニ ハッケン サレタ リュウモンガン : デイサイトシツ ヨウガンリュウ | |||||
出版者 | ||||||
出版者 | 特定非営利活動法人日本火山学会 | |||||
資源タイプ | ||||||
内容記述 | 論文(Article) | |||||
資源タイプ・ローカル | ||||||
雑誌掲載論文 | ||||||
資源タイプ・NII | ||||||
Journal Article | ||||||
資源タイプ・DCMI | ||||||
text | ||||||
資源タイプ・ローカル表示コード | ||||||
01 | ||||||
URL | ||||||
内容記述 | https://www.jstage.jst.go.jp/article/kazan/49/3/49_KJ00002524747/_article/-char/ja/ |