マントルの流れに対する抵抗は,オーストラリア上部マントルの電磁気衝突から推測される
1Geophysics Institute, University of Göttingen, Germany. f.simpson@gns.cri.nz
Nature
|August 9, 2001
まとめ
地震アニソトロピーは,オーストラリアの上層マントルのオリヴィン (olivine) のa-axesがプレート運動と整合していないことを明らかにします. これは,マントルが構造板の移動による変形に抵抗することを示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- ミネラル物理学 ミネラル物理学
- テクトニクス (地質学) とは
背景:
- オリヴィンの好ましい方向性によって引き起こされる地震性アニソトロピーは,シーア波分裂によってよく研究されています.
- オリビンの電気伝導性はアニソトロピーも示しているが,上層マントルの研究は稀である.
- マントルフローモデルは,オリヴィン (olivine) のa軸が,単純な剪定下でのプレート運動と並行することを予測しています.
研究 の 目的:
- オーストラリアの下の上層マントルの電気的アニソトロピーを調査するために.
- 電磁気衝撃を絶対的なプレート運動方向と比較するために.
- オリヴィン結晶のa軸とマントルの変形の並び方を推測する.
主な方法:
- オーストラリアの下の上層マントルの電磁画像.
- 地震アニソトロピーと電気伝導性の分析.
- プレートの絶対運動データとの比較.
主要な成果:
- マントルの電磁力衝突とオーストラリアのプレート運動方向の間の大きな不一致が観察されました.
- オリビン結晶のa軸は,現在の絶対プレート運動に平行して並行していない.
- この不整列は,マントルの変形に対する抵抗を示している.
結論:
- オリビンのa軸の平準化とプレート運動の仮定は,普遍的に成立しないかもしれません.
- マントルの変形はプレート運動によってのみ引き起こされるのではなく,他の抵抗力を示唆しています.
- 電気伝導性の研究は,上層マントルの動力学と鉱物組織を理解するために不可欠です.
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