1977年から1981年の間,セントヴィンセントのソフリエール (Soufriere) の変形研究
まとめ
ソフリエール火山は1979年4月の爆発前に徐々に膨張し,その後急速にデフレした. 遠くから見るとより大きな傾きは,地表から10km以上下にある深いマグマ室を示唆している.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 火山学 火山学とは
- ジオデシ (Geodesy) とは
背景:
- ソフリエール火山の噴火の歴史.
- 火山の動乱の予兆である.
研究 の 目的:
- 1979年4月の噴火前と後のソフリエール火山の地形変形を分析するために.
- 傾き測定に基づいて地下マグマシステムを推論する.
主な方法:
- 2つのステーションで乾燥傾斜の測定が行われました.
- 頂上から異なる距離での傾きデータの分析.
主要な成果:
- 最初の爆発の前に,少なくとも10マイクロラジアンの徐々に地面の膨張が観察されました.
- 活動開始後,20マイクロラジアンを超える急速なデフレーションが発生しました.
- 傾斜の大きさは,山頂から2.5kmの距離と比較して,6.5kmの距離で約2倍でした.
結論:
- 観測された変形パターンは,火山の下のマグマの移動と一致しています.
- 微分傾き測定は,深さ10km以上のマグマ室の存在を示唆しています.
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