まとめ
潜水板は,75~175kmの深さで,最大10~-1の相当なストレスを蓄積する. マントルの地震性により,この大きな膜がプレート沈没に起因する.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- テクトニクス (地質学) とは
背景:
- 潜水板は,アステノスフィアを通って沈むにつれて著しく変形します.
- これらのゾーンにおけるストレスの蓄積を理解することは,プレート構造モデルにとって極めて重要です.
研究 の 目的:
- 地震モメントの蓄積を用いて,スラブを潜水させる際の張力率を推定する.
- 板の変形におけるマントルの地震性の役割を調査する.
主な方法:
- ワダティ・ベニオフ・ゾーンにおける地震モメントの蓄積によるストレスの割合を推定する.
- 潜水板内の地震性のパターンを分析する.
主要な成果:
- 75~175kmの深さでは,毎秒約10~15の典型的なダウンディップのストレンスレートが見られました.
- 潜水板は,この深さの範囲で10~-1) 程度のストレスを蓄積します.
- マントルの地震性性は,スラブコアに大規模な膜菌株が蓄積されるための重要なメカニズムであるようです.
結論:
- 潜水板は,かなりの浸透変形を経験します.
- 観測されたスラブの形は,大きな膜株と一致しています.
- スラブは,表面の海洋プレートと比較して,より低い屈折硬さを示します.
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