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地磁気二極の強度と過去200万年の逆転率
Jean-Pierre Valet1, Laure Meynadier, Yohan Guyodo
1Géomagnétisme et Paléomagnétisme (UMR CNRS 7577), Institut de Physique du Globe de Paris, 4 Place Jussieu, 75252 Paris Cedex 05, France. valet@ipgp.jussieu.fr
Nature
|June 10, 2005
まとめ
200万年以上にわたる地磁気二極 Moment の進化は,反転しない期間中により強いフィールドを明らかにします. この研究は,ジオダイナモプロセスと地磁場行動に関する新しい洞察を提供します.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- パレオマグネティズム (古磁気学) とは
- 地球科学 地球科学 地球科学
背景:
- 地磁気二極 Moment の進化は,地磁気ダイナモのプロセスを理解するために重要です.
- 以前の再構築は,地磁気逆転を除いて,過去80万年に限られていた.
研究 の 目的:
- 過去200万年における地磁二極 Moment の進化を再構成する.
- ダイポールモメント強度と地磁気逆転の関係について調べる.
主な方法:
- 世界的な堆積物コアから相対的なパレオ強度に関する独立した記録を積み重ねる.
- 火山の溶岩からの絶対二極分数で複合曲線を校正する.
主要な成果:
- 過去200万年における地磁二極モメントの複合曲線が生成された.
- タイム・アヴェーレート・フィールドは,反転のない期間により強かった.
- 軸二極は逆転する前に60〜80kyr崩壊し,逆方向に急速に再構築します.
結論:
- より強い平均二極モメントは,遠回りや反転のような地磁気不安定性が少ないと相関する.
- 逆転を含む地磁場の振る舞いは,平均の磁場強度に関連しています.
- この研究は,地力力発電の過程に関する我々の理解を,さらに昔まで遡らせます.
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