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アンデス山脈の上昇の潜在的な原因として,ケノゾイク期の気候変動
1Department of Earth Sciences, Parks Road, Oxford, OX1 3PR, UK. simon.lamb@earth.ox.ac.uk
Nature
|October 24, 2003
まとめ
気候変動がアンデス山脈の上昇を促したのは,潜水地帯の動態に影響を与えることだったかもしれない. 気候によって引き起こされる堆積物の飢餓は,スイアストレスを増加させ,高いアンデス山脈を支えている.
科学分野:
- 地質学 地質学 地質学
- 気候科学 気候科学
- テクトニクス (地質学) とは
背景:
- 山の上昇は,逆ではなく,伝統的に気候変動と関連しています.
- アンデス山脈の形成は複雑で,石層の力が関与している.
研究 の 目的:
- ケノゾイク期の気候変動がアンデス山脈の上昇の原因となったメカニズムを提案する.
- 山の形成における潜水地帯のダイナミクスの役割を調査する.
主な方法:
- 南米の石層における力平衡の分析.
- 沈殿した堆積物,剪定ストレス,山の高さとの関係を調べる.
主要な成果:
- アンデス山脈の高度と地質学は,潜流ゾーンの剪定ストレスと浮力コントラストによって制御されます.
- サブダクションゾーンの切断ストレスは,潜水された堆積物の量に依存します.
結論:
- 気候に起因する侵食と沈殿物の堆積を制御するスブドクションと山の形成.
- 南米における気候制御による沈殿物の飢餓は,アンデス山脈の上昇を支える,高いシェアストレスを引き起こします.
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