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Updated: Feb 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

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地震学とダイヤモンドによる統一された大陸の厚さは,溶融で定義されたプレートを示唆しています

Saikiran Tharimena1, Catherine Rychert2, Nicholas Harmon2

  • 1Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK. s.tharimena@noc.soton.ac.uk.

Science (New York, N.Y.)
|August 12, 2017
PubMed
まとめ

大陸プレートには130~190kmの深さの明確な境界があり,おそらく部分的な溶融によって定義されています. この発見は地質学と地震学による 岩層の厚さに関するデータを 調和させています

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