地球の最下層マントルのMgSiO3ポストペロブスキート相の弾性

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Updated: Jul 24, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

T Iitaka1, K Hirose, K Kawamura

  • 1Computational Astrophysics Laboratory, RIKEN (The Institute of Physical and Chemical Research), 2-1 Hirosawa, Wako, Saitama 351-0198, Japan. tiitaka@riken.jp

Nature
|July 23, 2004
PubMed
まとめ

マグネシウムシリケートペロブスキート (MgSiO3) は,マントルの下部の唯一の構成要素ではないかもしれません. 新たに特定された"ペロブスキート後"段階は,地球の深い内部における地震の不連続性とアニソトロピーを説明する可能性がある.

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