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Updated: May 2, 2026

High-resolution Imaging of Nuclear Dynamics in Live Cells under Uniaxial Tensile Strain
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核-マントルの境界にある折りたたまれた,沈殿した石層の地震検出

Alexander R Hutko1, Thorne Lay, Edward J Garnero

  • 1Earth Sciences Department, University of California Santa Cruz, 1156 High Street, Santa Cruz, California 95064, USA. ahutko@pmc.ucsc.edu

Nature
|May 20, 2006
PubMed
まとめ

沈殿する海洋板は,地球の下層マントルに到達し,D'の地震不連続性のステップを作成します. このステップは,折りたたまれたスラブ材料が,コア-マントルの境界付近のペロブスキート後の相境界を変更することによって説明されます.

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