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Updated: Jun 10, 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

コア・マントルの境界から採取されたダイヤモンドのサンプルを羽根で採取した

Trond H Torsvik1, Kevin Burke, Bernhard Steinberger

  • 1Physics of Geological Processes and Geosciences, University of Oslo, Blindern, 0316 Oslo, Norway. trond.torsvik@ngu.no

Nature
|July 16, 2010
PubMed
まとめ

ダイヤモンドの主要な源であるキンベルライトの噴火は,深いマントルの構造と関連しています. 将来のダイヤモンド探査は,これらの安定した深層地帯を覆う古代のクレートンに焦点を当てなければなりません.

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