マグマの上昇とエトナ山の火山系の圧縮
Domenico Patanè1, Pasquale De Gori, Claudio Chiarabba
1Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Piazza Roma, 2, 95123 Catania, Italy. patane@ct.ingv.it
まとめ
エッナ山は,1994年から2001年の間にマグマ管道システムの急速な膨張と再圧縮を経験しました. これにより,地震が増加し,2002年10月以降の噴火を含む最近の爆発的な噴火が発生しました.
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:
- エトナ山は1991年から1993年にかけてデフレを示し,その後急激なインフレが続いた.
- 1994年以来のマグマの侵入は,1998年以降の山頂と側面の噴火をもたらしました.
研究 の 目的:
- 1994~2001年の地質学および地震変形データを分析する.
- エトナ山の最近の噴火活動を駆動する地下過程を理解するために.
主な方法:
- 地検データの分析 (地形変形).
- 地震変形データの分析. 地震変形データの分析.
- 地下マグマダイナミクスの解釈.
主要な成果:
- データによると,1994年から2001年の間,軸の侵入の周りの放射線圧縮が示されている.
- 証拠によると,エッナ山の配管システムが6〜15キロの深さで再圧縮されていることが示されています.
- この再圧縮は地震と火山の膨張を引き起こした.
結論:
- 地下マグマの侵入と再圧縮は,エトナ山の最近の爆発的な噴火の主要な原動力である.
- この発見は,深層マグマのダイナミクスと地表噴火の行動との関連を説明しています.
- 2002年の噴火は,エッナ山の歴史の中で最も爆発的な噴火の1つです.
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