新新生代卡里姆盆地的演化,北阿拉伯 - 努比亚盾牌
Haytham Sehsah1, Christopher L Kirkland2, Tim E Johnson2
1Geology Department, Faculty of Science, Damietta University, New Damietta, 34517, Damietta, Egypt. haytham_sehsah@du.edu.eg.
Scientific reports
|May 20, 2025
概括
卡里姆盆地 卡里姆盆地
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 沉积物学的沉积物学
背景情况:
- 阿拉伯-努比亚盾 (ANS) 经历了大约650万年前的大陆碰撞,形成了大盆地.
- 卡里姆盆地是ANS内的一个重要的合并后沉积中心,充满了约7公里的状沉积物.
研究的目的:
- 分析Kareim盆地的沉积阶段和构造演变在晚期新新生态时期的东非原生态.
- 解释沉积面和对盆地发展的构造学控制.
主要方法:
- 对面体协会和石形状的沉积物学分析.
- 对不一致性,断层和地平面关系的结构分析.
- 底酸 (detrital zircon) U-Pb 地质年代学,以限制盆地逆转时间.
主要成果:
- 盆地填充包括岩风扇到湖泊沉积物 (FA1-FA4),反映了不同的沉积环境.
- 确定了三个不同的沉积阶段,标志着不一致性和标志着构造逆转.
- 由推力断层和回收材料为特征的同沉积构造反转,发生在635万年前后.
结论:
- 卡里姆盆地记录了从初始沉降过渡到同碰撞的构造反转,最后到碰撞后的延伸.
- 盆地的演变与东非原生过程中西贡德瓦纳和东贡德瓦纳的合并密切相关.
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