地震による証拠は,地球の上層マントルの深部に水があることを示しています
Mark van der Meijde1, Federica Marone, Domenico Giardini
1Institute of Geophysics, Eidgenössische Technische Hochschule-Hönggerberg (HPP)/Swiss Federal Institute of Technology CH-8093 Zürich, Switzerland. mark@tomo.ig.erdw.ethz.ch
まとめ
深い上層マントルの水は,地震の不連続性に大きく影響する. 20〜35キロメートルの厚さの410キロメートルの不連続は,おそらく700ppmの水を含んでおり,マントルの移行ゾーンの性質に影響を与えます.
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
- ミネラル物理学 ミネラル物理学
背景:
- マントルのトランジションゾーン (MTZ) は地震の不連続を示している.
- 水分はマントルの性質と地震波の振る舞いに影響する重要な要因です.
研究 の 目的:
- 地震の不連続性に対する上層マントルの深層水の影響を調査する.
- 特定のMTZの不連続に起因する水分量を測定する.
主な方法:
- 変換された地震波の分析.
- 異質なマントル構造を通して地震波の伝播をモデル化.
主要な成果:
- 約410kmの深さで,厚さ20~35kmの地震断絶の証拠がある.
- この不連続性は,重量で百万分700分の1までと推定される,かなりの量の水の存在によって最もよく説明されます.
結論:
- 深い上層マントルの水は,地震の不連続性の性質を形作る上で重要な役割を果たします.
- 観測された410 kmの不連続性は,水性相の境界である可能性が高いか,水性鉱物によって影響されている.
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