ニラゴンゴ火山の建物の破裂によって引き起こされた前駆体のない噴火
D Smittarello1, B Smets2,3, J Barrière4
1European Center for Geodynamics and Seismology, Walferdange, Grand Duchy of Luxembourg. delphine.smittarello@ecgs.lu.
Nature
|August 31, 2022
まとめ
ニーラゴンゴ山
科学分野:
- 火山学
- 地理学
- 地化学
背景:
- 古典的な火山噴火モデルには 圧力の蓄積とマグマの上昇が含まれています
- 溶岩の湖がある 露天火山は 独特の監視の課題を 抱えています
- 2021年のニラゴンゴ山噴火は,典型的な前駆動モデルから逸脱した.
研究 の 目的:
- 2021年5月22日のナイラゴンゴ山の異常な側面噴火を調査する.
- 噴火の前駆物質とマグマの動きを 逆の順序で分析する
- 建物の破裂とそれに続く堤防の侵入の背後にあるメカニズムを理解する.
主な方法:
- 地質物理学的および地質化学的データの分析
- マグマの上昇と堤防の拡散をモデル化する.
- ナイラゴンゴ山の 2021 年の側面噴火のシーケンスの解釈.
主要な成果:
- ナイラゴンゴ山の噴火は 通常のマグマ上昇ではなく 建築物の破裂によって始まった
- 25キロメートルの堤防が ゴマ,ギセンイ,キブ湖の 浅瀬に浸透した.
- この噴火は前兆がなく,噴火後にマグマの動きがあった.
結論:
- この研究は,開いた風の火山に対する従来の噴火前駆モデルに挑戦しています.
- 都市噴出やリムニク噴出のような危険な出来事のリスクを強調しています.
- 浅いマグマシステムの有効な監視とリスク管理は依然として重要です.
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