リトスフィア-アステノスフィアの境界で観測された溶融豊かなチャンネル
1Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92093, USA. snaif@ucsd.edu
Nature
|March 23, 2013
まとめ
リトスフィア-アステノスフィアの境界線 (LAB) は部分的に溶けた層である可能性があり,プレート構造を説明します. 海洋プレートの下にあるこの低粘度ゾーンは,潤滑剤として作用し,溝の近くの沈下ダイナミクスを影響する.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- テキトノフィジックスの物理学です.
- マントルダイナミクス マントルダイナミクス
背景:
- 石層-アステノスフィアの境界線 (LAB) はプレート構造学にとって極めて重要ですが,その起源は議論されています.
- 地震研究は,LABでの速度不連続を示し,原因として部分的な溶解または脱水が提案されています.
研究 の 目的:
- ココス板の下にあるLABの電気伝導性を調査する.
- LABの物理的状態と起源を決定する.
主な方法:
- ニカラグア沖の海床磁気テラウリックデータ取得.
- LABでの電気伝導性のイメージング.
主要な成果:
- 高導電性層は,LABで45〜70kmの深さで特定されました.
- 導電性アニソトロピーは,板の運動に並行して切断された,管状の融解構造を示唆する.
結論:
- 若いプレートの下のLABは,部分的に溶けた層として解釈されます.
- この低粘度チャネルは,石層を分離し,板の動きを潤滑させ,沈殿に影響を与える可能性があります.
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