地球のマントルの弱い立方体CaSiO3ペロブスキート
J Immoor1, L Miyagi2, H-P Liermann3
1Bayerisches Geoinstitut (BGI), University of Bayreuth, Bayreuth, Germany.
Nature
|March 10, 2022
まとめ
キュービックカルシウムシリケート (CaSiO3) ペロブスキートは弱い下層マントル相である. 低強度と粘度がスラブの動態を制御し,地震の異常を説明する可能性があります.
科学分野:
- 地理学
- 鉱物物理学
- 高圧地化学
背景:
- 立方体CaSiO3のペロブスキットは,海底の地殻で約550kmの深さで形成される.
- 下層マントルのレオロジカルな性質は,まだよくわかっていない.
研究 の 目的:
- 立方体CaSiO3ペロフスキットのプラスチック強さとリオロジック行動を調べる.
- プレートダイナミクスと下層マントルの構造におけるその役割を決定する.
主な方法:
- 立方CaSiO3ペロブスキットのプラスチック強度測定
- マントルの下部状態をシミュレートする高圧および高温のシミュレーション (深さ~1200 km).
主要な成果:
- 立方CaSiO3ペロブスキットは,より低いマントルの温度でブリッジマニットとフェロペリクラゼよりも著しく弱い.
- その強度と粘性は,他の主要な下層マントル相よりもかなり低い.
- 下層マントルの 最弱の相として特定された.
結論:
- 弱い立方体CaSiO3ペロブスキットは,おそらくスラブダイナミクスを支配する.
- 海殻をマントルから分離するメカニズムです
- 最下層マントルとコアマントルの境界にある低地震速度の領域を説明できる.
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