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Updated: May 30, 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

ウィルソン周期の始まりは,次大陸のマントルのダイヤモンドによって示された 3 億年です

Steven B Shirey1, Stephen H Richardson

  • 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA. shirey@dtm.ciw.edu

Science (New York, N.Y.)
|July 23, 2011
PubMed
まとめ

ダイヤモンドに含まれる鉱物含有物は,約30億年前,地球のマントルの主要な組成の変化を明らかにします. この変化,ペリドートイチス型からエコロジチス型のダイヤモンドへの変化は,プレートテクトニクスの初期発生を意味しています.

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