ジオイドル変化とホロセンの河口に沿った岸面の傾き:セネガル川地域,西アフリカ
まとめ
セネガル河口の海洋堆積物は,古代の海面を明らかにしています. 復元された古ジオイドは,大陸の縁の傾きが最小で,地質モデルに挑戦しています.
科学分野:
- 地質学 地質学 地質学
- マリンサイエンス マリンサイエンス・サイエンス
- パレオジオグラフィー パレオジオグラフィー
背景:
- 過去の海面の変化を理解することは,将来の沿岸への影響を予測するのに不可欠です.
- 大陸の縁の傾きは,沿岸の地形学と海面記録に影響する.
研究 の 目的:
- セネガル河口の古生物学者を再構築するために.
- 過去6500年にわたる大陸の縁の傾きの大きさを評価する.
主な方法:
- 海洋堆積物のサンプル採取のためのフィールド遠征.
- 地質学的サンプルのレベルリングと年代測定.
- パレオゲオイドの再構築は,日付のついたサンプルを用いて行われました.
主要な成果:
- 現在より6500,5500,そして1800年前のパレオジオイドを再構築.
- 測られた大陸縁の傾きは1メートル未満.
- 傾きは海岸から内陸まで120kmの横断で測定された.
結論:
- 観測された傾きは,いくつかの数学的モデルによって予測されたより大幅に少ない.
- この地域の海面再建は,傾斜の誤差1メートル以内で信頼性があります.
- Rhéomargeプロジェクトは,西アフリカの古地理学にとって貴重なデータを提供しています.
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