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Updated: Jun 30, 2026

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Electric and Magnetic Field Devices for Stimulation of Biological Tissues
Published on: May 15, 2021
アンデス山脈の上昇
Carmala N Garzione1, Gregory D Hoke, Julie C Libarkin
1Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA. garzione@earth.rochester.edu
まとめ
山岳帯の高さの変化は,徐々にではなく,急速に起こります. この急速な表面の上昇は,地殻の加厚後の密度の高い下層石層の除去によって引き起こされる.
科学分野:
- 地質学 地質学 地質学
- テクトニクス (地質学) とは
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 山岳帯は,地殻の縮小と加厚により,通常,徐々に上昇する.
- 以前のモデルでは,山の形成の継続的な上昇過程を想定していました.
研究 の 目的:
- 山岳帯における地表上昇の動態を調査する.
- 徐々に山が形成されるという伝統的見解に異議を唱えるため.
主な方法:
- アンデス山脈からの地質学的データの分析.
- 地質学的時間スケールにおける高さの変化の再構築.
主要な成果:
- アンデス山脈の上昇は,何百万年もの間,安定したままでした.
- 急速な標高変化 (1~4百万年で1.5km以上) が観察されました.
- Uplift イベントは,断続的で迅速です.
結論:
- 山岳帯の上昇は,常に漸進的とは限らない.
- 表面の急速な上昇は,密度の高い下層石層の除去と関連しています.
- このプロセスは,長期にわたる地殻と石層マントルの厚み化に続く.
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