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Updated: Jun 3, 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

地球の深層マントルのレドックス凍結と融解は,炭素と鉄のレドックス結合によるものです

Arno Rohrbach1, Max W Schmidt

  • 1Institut für Geochemie und Petrologie, ETH Zürich, Sonneggstrasse 5, 8092 Zürich, Switzerland. arno.rohrbach@gmail.com

Nature
|March 29, 2011
PubMed
まとめ

炭酸塩による地表深層の融解が地球に起因している.

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