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{"_buckets": {"deposit": "ad106a16-d049-4566-b4c1-5d1e44965cdd"}, "_deposit": {"id": "5571", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5571"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005571", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2004-02", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "106", "bibliographicPageStart": "103", "bibliographicVolumeNumber": "80", "bibliographic_titles": [{"bibliographic_title": "Proceedings of the Japan Academy Series B: Physical and Biological Sciences", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "In 1707, approximately 0.7 km3 of magma erupted from new vents on the southeastern slope of Fuji volcano. The air-fall clasts of this explosive eruption are composed of vesicular dacite pumice, andesitic dense scoria, basaltic dense scoria, and vesiculated basalt scoria, stratified from bottom to the top of the fallout unit. Some compositional gaps are found in the variation from basalt to dacite indicating that three independent magmas, basalt, andesite and dacite, existed just prior to the eruption. Andesite and dacite magmas are mixed just prior to or during the eruption showing a linear two component mixing in the major and trace element concentration. Basalt in the later stage of the eruption shows no compositional affinity with the above two magmas. Basalt magma might have acted as a heat source to remobilize the andesite and dacite magmas, and the explosive eruption of basalt could have been caused by the abrupt pressure release due to precursory mixing and eruption of dacite and andesite magmas.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.2183/pjab.80.103"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0386-2208", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Mitsuhiro Yoshimoto", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Toshitsugu Fujii", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Takayuki Kaneko", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Atsushi Yasuda", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Setsuya Nakada", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Multiple magma reservoirs for the 1707 eruption of Fuji volcano, Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Multiple magma reservoirs for the 1707 eruption of Fuji volcano, Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5571", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5571", "relation": {}, "relation_version_is_last": true, "title": ["Multiple magma reservoirs for the 1707 eruption of Fuji volcano, Japan"], "weko_shared_id": -1}
  1. 防災科研関係論文

Multiple magma reservoirs for the 1707 eruption of Fuji volcano, Japan

https://nied-repo.bosai.go.jp/records/5571
https://nied-repo.bosai.go.jp/records/5571
b00f5e12-5874-43f3-b046-deb87934f9b4
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Multiple magma reservoirs for the 1707 eruption of Fuji volcano, Japan
言語
言語 eng
著者 Mitsuhiro Yoshimoto

× Mitsuhiro Yoshimoto

en Mitsuhiro Yoshimoto

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Toshitsugu Fujii

× Toshitsugu Fujii

en Toshitsugu Fujii

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Takayuki Kaneko

× Takayuki Kaneko

en Takayuki Kaneko

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Atsushi Yasuda

× Atsushi Yasuda

en Atsushi Yasuda

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Setsuya Nakada

× Setsuya Nakada

en Setsuya Nakada

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抄録
内容記述タイプ Other
内容記述 In 1707, approximately 0.7 km3 of magma erupted from new vents on the southeastern slope of Fuji volcano. The air-fall clasts of this explosive eruption are composed of vesicular dacite pumice, andesitic dense scoria, basaltic dense scoria, and vesiculated basalt scoria, stratified from bottom to the top of the fallout unit. Some compositional gaps are found in the variation from basalt to dacite indicating that three independent magmas, basalt, andesite and dacite, existed just prior to the eruption. Andesite and dacite magmas are mixed just prior to or during the eruption showing a linear two component mixing in the major and trace element concentration. Basalt in the later stage of the eruption shows no compositional affinity with the above two magmas. Basalt magma might have acted as a heat source to remobilize the andesite and dacite magmas, and the explosive eruption of basalt could have been caused by the abrupt pressure release due to precursory mixing and eruption of dacite and andesite magmas.
言語 en
書誌情報 en : Proceedings of the Japan Academy Series B: Physical and Biological Sciences

巻 80, 号 2, p. 103-106, 発行日 2004-02
ISSN
収録物識別子タイプ ISSN
収録物識別子 0386-2208
DOI
関連識別子 10.2183/pjab.80.103
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