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第"原則は,下層マントルの鉱物および弱いD'層における拡散の制約である

M W Ammann1, J P Brodholt, J Wookey

  • 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK. m.ammann@ucl.ac.uk

Nature
|May 28, 2010
PubMed
まとめ

ポストペロブスキート (MgSiO3) のイオン拡散は高度にアニソトロピックであり,地球のD'層のこの鉱物を著しく弱体化させます. これは地震観測を説明し,コアとマントルの相互作用と熱流に影響を与える.

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