イエローストーン:化学マントルの羽根の地震的証拠
まとめ
地震波は,イエローストーン・カルデラの下にある化学マントルの羽根を明らかにしている. このプラームには高速なコアと低速度なコラーがあり,地震波の移動時間に影響を与えます.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- 火山学 火山学とは
背景:
- イエローストーン・カルデラは,火山活動と地熱活動が顕著な地域です.
- 地下構造を理解することは,火山の危険性を評価する上で極めて重要です.
研究 の 目的:
- イエローストーン・カルデラの下の深い地表構造を調査するために.
- 地震移動時間の変動を引き起こす異常の性質を決定する.
主な方法:
- ネバダ州試験場からの地震P波の分析.
- 円筒状の構造を用いて地震の移動時間異常をモデル化する.
主要な成果:
- 地震波は,特定の深さでイエローストーン・カルデラの下を通過する際,移動時間の異常を示した.
- 高速コアと低速コラーを備えた垂直の円筒形構造がモデル化されました.
- この構造は200から400キロメートルの深さまで広がっています.
結論:
- モデル化された地震速度の構造は,化学マントルの羽根と一致しています.
- この発見は,イエローストーン・カルデラの下にあるマントル・プルームの存在を裏付けている.
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