垂直的に広範囲で不安定なマグマ系:火山性過程の統一された見方
Katharine V Cashman1, R Stephen J Sparks2, Jonathan D Blundy2
1School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK. glkvc@bristol.ac.uk.
まとめ
火山の噴火は 地球に広がるマグマによって引き起こされる
科学分野:
- 地球科学
- 火山学
- マグマティック・システム
背景:
- 古典的な研究は上層の地殻のマグマ室に焦点を当てた.
- 最近の研究では,地殻全体にわたってマグマの過程を強調しています.
研究 の 目的:
- トランスクラスタルマグマティックシステムの証拠を検証する.
- 溶融層の安定性と不安定性を支配する物理的プロセスを強調する.
- 溶融の上昇と浅いマグマ室の形成の条件を調査する.
主な方法:
- 地質学的および地物理学的証拠の文献レビュー.
- マグマ系における物理的過程の分析
- 溶融生成,分離,および蓄積に関するデータの合成.
主要な成果:
- 低層から高層まで,地殻全体で活動しています.
- 低地殻の融解と高地殻の急速な蓄積のバランスがある.
- 地殻の融解の物理的状態,分布,長寿をめぐって活発な議論が行われています.
結論:
- 火山活動を理解するために,地殻を越えたマグマ系は極めて重要です.
- 低地殻の溶けた層の不安定化は,浅いマグマ室の形成につながります.
- 浅いマグマ室は 火山噴火で重要な役割を果たします
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