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  1. 防災科研関係論文

Rapid growth and catastrophic destruction events of Planchón Volcano, Southern Andes

https://nied-repo.bosai.go.jp/records/6775
https://nied-repo.bosai.go.jp/records/6775
251a829d-bd1c-4c5e-b12a-4985b2851739
Item type researchmap(1)
公開日 2024-09-16
タイトル
言語 en
タイトル Rapid growth and catastrophic destruction events of Planchón Volcano, Southern Andes
言語
言語 eng
著者 José Antonio Naranjo

× José Antonio Naranjo

en José Antonio Naranjo

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Jorge Romero

× Jorge Romero

en Jorge Romero

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Juan Pablo Contreras

× Juan Pablo Contreras

en Juan Pablo Contreras

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Yuji Orihashi

× Yuji Orihashi

en Yuji Orihashi

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Kevin Scott

× Kevin Scott

en Kevin Scott

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Miguel Haller

× Miguel Haller

en Miguel Haller

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Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

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抄録
内容記述タイプ Other
内容記述 During the Late Pleistocene-to-Holocene, the mafic Planchón volcano (35.2 °S, Southern Andes) experienced two important destructive events: a sector collapse to the west and a multiphase explosive eruption transforming the east summit area. We provide new field and laboratory evidence, including geochemical, geochronologic, and geological-morphological analysis, to reconstruct the evolution, triggering mechanisms, and physical parameters of these events.The lateral collapse (48~ka BP) was mainly predisposed by a tectonically westward-inclined substratum and rapid edifice growth rates (0.3–0.48 km3 ka-1). The resulting Planchón-Teno debris avalanche became valley-confined traveling at c. 260 km h-1 up to 95 km distance and forming an 8.6 ± 1.3 km3 deposit. The resulting 4.1 km wide amphitheater was later destroyed at c. 7 ka BP by the multiphase Valenzuela phreatomagmatic eruptions, forming a c. 2.5 km diameter caldera. The case of the Planchón volcano warns that rapidly growing mafic volcanoes imply a substantial catastrophic hazard increase for the surrounding areas.
言語 en
書誌情報 en : Volcanica

巻 7, 号 1, p. 21-49, 発行日 2024-01-30
出版者
言語 en
出版者 Volcanica
ISSN
収録物識別子タイプ EISSN
収録物識別子 2610-3540
DOI
関連識別子 10.30909/vol.07.01.2149
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