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Updated: May 2, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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地殻におけるマグマの化学的分化,冷蔵,再移動

M D Jackson1, J Blundy2, R S J Sparks2

  • 1Department of Earth Science and Engineering, Imperial College London, London, UK. m.d.jackson@imperial.ac.uk.

Nature
|December 5, 2018
PubMed
まとめ

マグママッシュ貯蔵庫の反応性溶融流は,異なるマグマの形成と古い結晶の貯蔵を説明します. このプロセスは火山地質学と火山学における伝統的なマグマ室モデルに 挑戦しています

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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