ペロブスキート後のMgSiO3の滑り系:D'アニソトロピーの影響
Lowell Miyagi1, Waruntorn Kanitpanyacharoen, Pamela Kaercher
1Department of Geology and Geophysics, Yale University, New Haven, CT 06511, USA.
まとめ
MgSiO(3) は, (001) 面でのペロブスキート転落後,地球の下層マントルの地震性アニソトロピーを強化する. これにより,D'層における変形メカニズムと地震の解釈が明確になります.
科学分野:
- ミネラル物理学 ミネラル物理学
- 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
背景:
- 最下層マントルの鉱物相の変形は,地震性アニソトロピーの解釈に極めて重要です.
- MgSiO ((3)) のペロブスキート後の変形による滑りについて論争がある.
研究 の 目的:
- 高圧下でのペロブスキート後のMgSiO ((3) の変形機構と好ましい方向性を調査する.
- 地球のD''領域における地震性アニソトロピーの生成におけるスリップの役割を明確にするために.
主な方法:
- 地球の下層マントルの条件をシミュレートする高圧実験.
- 格子平面の向きと好みの向きの進化を観察するためのX線 difraktion.
- 実験結果に基づく変形とアニソトロピーのモデリング.
主要な成果:
- MgSiO(3) ポストペロブスキット (001) 格子平面の方向性を高角度から圧縮ポスト変換に示します.
- 偏向の強度は,圧縮で148 GPaから185 GPaに大幅に増加し, (001) スリップを示します.
- 結果は,以前の研究と対照的に,単に相変換ではなく,偏った方向性を変形に代入します.
結論:
- (001) 格子平面の滑り方は,下層マントルの条件下で,MgSiO ((3)) のペロブスキート後の変形のための重要なメカニズムです.
- この発見は,地震性アニソトロピーの解釈,特にD'領域におけるシーザー波分裂の解釈を支持する.
- この研究は,鉱物の行動と地球の深い内部における地震波の伝播に関する私たちの理解を洗練します.
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