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在过去的2300万年中,红海东北部碳酸盐平台的演变
Tihana Pensa1, Guillaume Baby2, Thomas Teillet1
1Physical Science and Engineering, King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.
Scientific reports
|March 26, 2025
概括
米甸半岛展现了米奥生碳酸盐平台,这些平台从软体动物坡道演变为珊瑚藻平台,由于盐度高,生产暂停,然后在米奥生晚期恢复.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 在平流图学上,平流图学是平流图学.
背景情况:
- 麦迪安半岛提供独特的,连续暴露的下至中米欧时代的协同裂变沉积层.
- 这些层包括保存得非常好的碳酸盐平台,对于了解红海裂变至关重要.
研究的目的:
- 调查碳酸盐平台形态,结构设置和红海东北部分布的变化.
- 为了将这些平台置于红海裂的构造学和古地理演变中的背景.
主要方法:
- 整合了表面观测,地质物理数据和井日志.
- 应用 (Sr) 同位素层学来准确测年.
- 对平台演变的分析,从早期的同步裂变到晚期的同步裂变阶段.
主要成果:
- 从贝类主导的坡道向珊瑚和藻类主导的平台的过渡发生在同步裂变阶段 (23-14 Ma).
- 碳酸盐的产量在中和上米欧纪 (13-6万年前) 之间停止,原因是盐度过高.
- 碳酸盐生产在米奥生 (5.5万年) 末期恢复,厚厚的平台受到盐构造学的影响.
结论:
- 这项研究揭示了红海裂中苗代碳酸盐平台的动态进化.
- 盐构造学在塑造后期平台发展方面发挥了重要作用.
- 了解这些古老的平台,可以了解裂盆地演变和碳酸盐工厂对环境变化的反应.
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