沿着全新世纪河口的地形变化和海岸水平倾斜:塞内加尔河区,西非
概括
塞内加尔河口的海洋沉积物揭示了古代的海平面. 重建的古地质体显示了极小的大陆边缘倾斜,挑战了地质模型.
科学领域:
- 地质地质地质地质地质地
- 海洋科学 海洋科学
- 古地质学 古地质学
背景情况:
- 了解过去的海平面变化对于预测未来沿海影响至关重要.
- 大陆边缘倾斜影响沿海地形学和海平面记录.
研究的目的:
- 为了重建塞内加尔河口的古地质.
- 为了评估过去6500年的大陆边缘倾斜幅度.
主要方法:
- 实地探险为采集海洋沉积物的样本.
- 地质样品的平衡和约会.
- 使用已知日期的样本进行古地质体重建.
主要成果:
- 在现在之前6500,5500和1800年的重建古地质.
- 测量的大陆边缘倾斜小于1米.
- 倾斜度测量了从海岸到内陆的120公里横断.
结论:
- 观察到的倾斜幅度明显低于一些数学模型预测的.
- 该地区的海平面重建可靠,倾斜误差为1米.
- 雷奥马尔吉项目为西非古地理学提供了有价值的数据.
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