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Updated: May 6, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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中部アンデスで発生する潜水と衝突の過程は,変換された地震相によって制約されています

X Yuan1, S V Sobolev, R Kind

  • 1GeoForschungsZentrum Potsdam, Telegrafenberg, Germany.

Nature
|January 5, 2001
PubMed
まとめ

深層地震画像は,地殻の厚みだけでなく,石層マントルの薄れが,高い中央アンデス山脈に寄与したことを明らかにしています. また,この研究は,納スカプレートにおける遅延型変異反応の証拠も提供しています.

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