まとめ
火山の弧から噴火するアンデサイトは,マントルの深いプロセスと関連している. アンデシト火山活動のためのマグマ生成は,中程度の深さの地震とベニオフ地震地帯と関連しています.
科学分野:
- 地質学 地質学 地質学
- 火山学 火山学とは
- 地震学 地震学とは
背景:
- 環太平洋のアンデサイト,ベサルト,ダサイトは,島の弧や大陸の山脈から噴出しています.
- 火山の弧の位置は,溝の隣接する浅い地震帯と相関しています.
研究 の 目的:
- 環太平洋の亜地殻起源とエシト火山の起源を調査する.
- 火山活動と地震データ,マントルの構造を相関させるため.
主な方法:
- 火山の弧と地震地帯の地質地図作成.
- 噴火した溶岩の組成,特にポータシュの含有量の分析.
- 地震トモグラフィーは,ベニョフゾーンや低速度ゾーンなどの地殻下構造を図示する.
主要な成果:
- 活発な火山は,ベニョフゾーンとグーテンベルク低速ゾーンの交差点によって定義される地殻下部の領域の上に並びます.
- 溶岩のポータシュ含量とベニオフゾーンの深さには強い相関関係がある.
- アンデシト火山は,マントルに起源があるようです.
結論:
- アンデシト火山は,マントルのプロセスと関連している.
- ベニオフゾーンの中間の焦点深さの地震は,マグマ生成と関連しています.
- ベニオフゾーンの深さは,噴火した溶岩の組成に影響します.
関連する概念動画
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