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Updated: Jul 8, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Published on: August 5, 2016

古い山の地殻の根元にある浮力力が弱まっている

Karen M Fischer1

  • 1Department of Geological Sciences, Brown University, Providence, Rhode Island 02912, USA. Karen_Fischer@brown.edu

Nature
|June 28, 2002
PubMed
まとめ

山地殻の根は,冷却により何百万年にもわたって浮力を失い,侵食が山々を磨くにつれて地形を支える能力を低下させます. これは,古い山が,地殻の根に比べて,より小さなリリエフを持っている理由を説明します.

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