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  1. 防災科研関係論文

Noble gas isotopes reveal degassing-derived eruptions at Deception Island (Antarctica): implications for the current high levels of volcanic activity

https://nied-repo.bosai.go.jp/records/2914
https://nied-repo.bosai.go.jp/records/2914
50a0e820-1b56-4058-ab78-53e79d670011
Item type researchmap(1)
公開日 2023-12-26
タイトル
言語 en
タイトル Noble gas isotopes reveal degassing-derived eruptions at Deception Island (Antarctica): implications for the current high levels of volcanic activity
言語
言語 eng
著者 Antonio M. Álvarez-Valero

× Antonio M. Álvarez-Valero

en Antonio M. Álvarez-Valero

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Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

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Antonio Caracausi

× Antonio Caracausi

en Antonio Caracausi

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Antonio Polo Sánchez

× Antonio Polo Sánchez

en Antonio Polo Sánchez

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Ray Burgess

× Ray Burgess

en Ray Burgess

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Adelina Geyer

× Adelina Geyer

en Adelina Geyer

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Javier Borrajo

× Javier Borrajo

en Javier Borrajo

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José A. Lozano Rodríguez

× José A. Lozano Rodríguez

en José A. Lozano Rodríguez

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Helena Albert

× Helena Albert

en Helena Albert

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Meritxell Aulinas

× Meritxell Aulinas

en Meritxell Aulinas

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Elena Núñez-Guerrero

× Elena Núñez-Guerrero

en Elena Núñez-Guerrero

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抄録
内容記述タイプ Other
内容記述 Abstract

Deception Island is one of the most active volcanoes in Antarctica with more than twenty explosive eruptions in the past two centuries. Any future volcanic eruption(s) is a serious concern for scientists and tourists, will be detrimental to marine ecosystems and could have an impact to global oceanographic processes. Currently, it is not possible to carry-out low and high frequency volcanic gas monitoring at Deception Island because of the arduous climatic conditions and its remote location. Helium, neon and argon isotopes measured in olivine samples of the main eruptive events (pre-, syn- and post caldera) offer insights into the processes governing its volcanic history. Our results show that: (i) ascending primitive magmas outgassed volatiles with a MORB-like helium isotopic signature (<sup>3</sup>He/<sup>4</sup>He ratio); and (ii) variations in the He isotope ratio, as well as intensive degassing evidenced by fractionated <sup>4</sup>He/<sup>40</sup>Ar<sup>*</sup> values, occurred before the beginning of the main eruptive episodes. Our results show how the pre-eruptive noble gas signals of volcanic activity is an important step toward a better understanding of the magmatic dynamics and has the potential to improve eruption forecasting.
言語 en
書誌情報 en : Scientific Reports

巻 12, 号 1, p. 19557, 発行日 2022-11-15
出版者
言語 en
出版者 Springer Science and Business Media LLC
ISSN
収録物識別子タイプ EISSN
収録物識別子 2045-2322
DOI
関連識別子 10.1038/s41598-022-23991-3
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