集水域から地球規模にわたる 1 億年の景観の動態
Tristan Salles1, Laurent Husson2, Patrice Rey1
1School of Geosciences, The University of Sydney, Sydney, Australia.
まとめ
この研究では 地球の過去景観を 1億年以上にわたって グローバルモデルを使って再構築しています 安定したケノゾイク期の沈殿率を明らかにし,陸から海への沈殿物の移転の明確な段階を示しています.
科学分野:
- 地球科学
- 古代地理学
- 地形学
背景:
- 古代地球を再現するには 過去の風景を理解することが重要です
- 地球規模の景観の進化モデルは この再構築のための不可欠なツールです
研究 の 目的:
- 地球システムの重要なメトリックを定量化するために, グローバル生理学,堆積物流量,および階層構造を含む.
- 海への沈殿物の流出を制御する表面過程の役割を再評価する.
主な方法:
- 地球規模の景観の進化モデルを用いて
- 過去1億年にわたる古高層構造と古気候を再構築
主要な成果:
- 地球システムの重要なメトリックの継続的な定量化
- 定着率はケノゾイク全体で安定した.
- 陸地から海洋盆地への沈殿物の移転の異なる段階を特定する.
結論:
- このモデルは,地質学的記録と再構築の不一致を特定するためのツールを提供します.
- 地表の過程は 安定して段階的に 沈殿物を海に運ぶ役割を果たします
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