断層や地質学的なストレスにより,マグマが急激に堤防に流入する
Freysteinn Sigmundsson1, Michelle Parks2, Halldór Geirsson1
1Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland.
まとめ
巨大なマグマが堤防に侵入すると 低圧で発生し 大きな経路が開き ストレスが蓄積されます これはマグマの急速な流れと 噴火の危険性を説明します
科学分野:
- 地質学
- 火山学
- 地理学
背景:
- 巨大な堤防の群れは 広範囲の横断的なマグマの流れを示し,しばしば数百キロメートルを超える.
- 急速なマグマ流出を促すメカニズムを理解することは,危険性の評価に不可欠です.
研究 の 目的:
- 大量のマグマが わずかな圧力で 堤防に流れる条件を説明するために
- 最近の堤防の侵入で観測された急速な初期マグマの流れをモデル化するために.
主な方法:
- マグマ流動のダイナミクスの数値モデル化
- 堤防の経路に沿ったストレスの蓄積の分析
- 2023年11月のグリンダビック堤防の侵入事例
主要な成果:
- 大量のマグマが堤防に流れ込むのは,大きな経路が開き,張力圧力が徐々に増加すると,適度な過圧で可能です.
- モデル化された初期フローレットは約7400立方メートル/秒で約15kmの堤防に達した.
- グリンダビークの堤防の侵入は,このプロセスの重要な例です.
結論:
- この研究は,ダイクが急速に広がり,マグマが大量に流れていく仕組みを提供する.
- 高流量侵入は重大な危険性を持ち,表面噴火につながる可能性があります.
- 大規模な堤防の形成と 付随する火山の危険性についての洞察を 提供しています
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