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  1. 防災科研関係論文

Precursory activity and evolution of the 2011 eruption of Shinmoe-dake in Kirishima volcano-insights from ash samples

https://nied-repo.bosai.go.jp/records/5887
https://nied-repo.bosai.go.jp/records/5887
ccaaa78c-328d-42f8-92d0-fda3725936e4
Item type researchmap(1)
公開日 2023-05-24
タイトル
言語 en
タイトル Precursory activity and evolution of the 2011 eruption of Shinmoe-dake in Kirishima volcano-insights from ash samples
言語
言語 eng
著者 Yuki Suzuki

× Yuki Suzuki

en Yuki Suzuki

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Masashi Nagai

× Masashi Nagai

en Masashi Nagai

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Fukashi Maeno

× Fukashi Maeno

en Fukashi Maeno

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Atsushi Yasuda

× Atsushi Yasuda

en Atsushi Yasuda

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Natsumi Hokanishi

× Natsumi Hokanishi

en Natsumi Hokanishi

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Taketo Shimano

× Taketo Shimano

en Taketo Shimano

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Mie Ichihara

× Mie Ichihara

en Mie Ichihara

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Takayuki Kaneko

× Takayuki Kaneko

en Takayuki Kaneko

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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 After a precursory phreatic stage (2008 to 2010), the 2011 Shinmoe-dake eruption entered a phreatomagmatic stage on January 19, a sub-Plinian and lava accumulation stage at the end of January, a vulcanian stage in February-April, and a second phreatomagmatic stage in June-August. Component ratio, bulk composition, and particle size of the samples helped us define the eruptive stages. The juvenile particles were first found in the January 19 sample as pumice (8 vol%) and were consistently present as scoria and pumice particles thereafter (generally similar to 50 vol%, decreasing in weaker events). The January 19 pumice has water-quench texture. After the lava accumulation, particles of that lava origin came to account for 30 similar to 70 vol% of the ash. The second phreatomagmatic stage is proposed because of fine ash and long eruption period. The SiO2 contents of bulk ash are lower in post-January 19, 2011 eruptions, reflecting lower average SiO2 contents in 2011 ejecta than in past ejecta. The free-crystal assemblages were two pyroxenes + plagioclase + Fe-Ti oxides until 2010; olivine joined the assemblage in 2011, when juvenile ash was erupted. This change is consistent with the absence or smaller sizes of olivine phenocrysts in past ejecta.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 65, 号 6, p. 591-607, 発行日 2013
出版者
言語 en
出版者 TERRA SCIENTIFIC PUBL CO
ISSN
収録物識別子タイプ ISSN
収録物識別子 1343-8832
DOI
関連識別子 10.5047/eps.2013.02.004
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