複数の貯水池間のマグマ移動が噴火サイクルに及ぼす影響
Derek Elsworth1, Glen Mattioli, Joshua Taron
1College of Earth and Mineral Sciences, Penn State University, University Park, PA 16802, USA. elsworth@psu.edu
まとめ
火山の噴火は偶発的なものです. Soufrière Hills火山内のマグマの移転は,中部地殻の貯水池を栄養する継続的な深い供給を示しており,これは時折地表噴火を助長します.
科学分野:
- 火山学 火山学とは
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 火山噴火は連続したマグマ供給にもかかわらず,エピソード的です.
- マグマ移動のダイナミクスを理解することは,噴火の予測に不可欠です.
研究 の 目的:
- シュフリエールヒルズ火山内のマグマの移転を地質学的にイメージするために.
- 断続的な火山噴火を引き起こすメカニズムを調査する.
主な方法:
- マグマ流出と表面変形の歴史の分析.
- 地表層の深い水道管の地質画像撮影.
主要な成果:
- 深い地殻とマントルからのマグマの継続的な供給が観察されました.
- マグマの移動は,地殻の中央の貯水池 (約. 12km) の浅い貯水池 (約. 6km) でした.
- エピソード的噴火は,浅い貯水池の下にあるマグマのエピソード的"バルブ"と関連付けられました.
結論:
- Soufrière Hills火山は,継続的な深いマグマ供給システムで動作しています.
- エピソード的噴火は,マグマのエピソード的移動によって制御されます.
- 概念的なモデルは,バルブ状の中間地殻のマグマ貯水池を通して火山の周期性を説明します.
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