东欧的沉积盆地长期被色的地幔所加热,上升
Alik Ismail-Zadeh1, Anne Davaille2, Jean Besse3
1Karlsruhe Institute of Technology, Institute of Applied Geosciences, Karlsruhe, Germany. alik.ismail-zadeh@kit.edu.
Nature communications
|May 9, 2024
概括
珀姆异常,在东欧下方涌起的深层地幔,影响了石质层的演化和碳化合物盆地形成,持续了1.5亿到2亿年. 这项地幔羽毛动力学研究揭示了它在为碳化合物成熟创造条件方面的作用.
科学领域:
- 地质物理学 地质物理学
- 地力学是什么?地力学是什么?
- 石油地质学 石油地质学
背景情况:
- 在东欧平台下方的核心-地幔边界处的负地震速度异常 (Perm Anomaly) 与深层地幔上升有关.
- 这种上升与东欧石化层的过去相互作用及其表面效应仍然不清楚.
研究的目的:
- 为了研究珀姆异常上升和东欧石化层之间的长期相互作用.
- 了解这种相互作用对沉积盆地和碳化合物生成的演变的影响.
主要方法:
- 幔子羽毛模拟模拟上升的动态.
- 全球板块运动重建以追踪东欧平台的位置.
- 分析模型的热传导通过石质层.
主要成果:
- 东欧石化层可能在减弱的珀姆异常上升上居住了1.5亿至2亿年.
- 富含碳化合物的盆地的垂直构造运动显示,当平台移动在罗纪后的异常上时,出现了升起或最小沉降.
- 这些盆地的长期缓慢加热由上游产生,为碳化合物成熟创造了有利的条件.
结论:
- 在地幔羽毛动力学,盆地演化和碳化合物生成之间存在着显著的关系.
- 珀姆异常在塑造东欧平台的地质历史和资源潜力方面发挥了关键作用.
- 了解地球深层的过程对于探索碳化合物系统至关重要.
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