概括
原始通过海洋和大陆地逃离地球的地幔,而次大陆脱气与活跃的地延伸有关. 这个过程挑战了当前关于地球热量和平衡的模型.
科学领域:
- 地质化学 地质化学
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
背景情况:
- 自地球形成以来被困的原始,通过新的海洋地脱气.
- 与预期相反,通过大陆地也发生了大量的脱气.
研究的目的:
- 为了研究人们对脱气的次大陆过程的了解不足.
- 为了将被观察到的地幔热量损失率与损失相协调.
主要方法:
- 对地幔挥发性物质通过大陆地逃逸的分析,特别是在西欧.
- 损失率与从和中产生放射性热量的比较.
主要成果:
- 西欧地幔挥发性逃逸与活跃的地扩展有关.
- 目前的地幔热损失速度明显高于损失速度 (因数为20).
结论:
- 亚大陆脱气是一个重要的过程,发生在地正在积极扩展的地方.
- 热量和损失率的差异表明地幔中的积累或地球散热化学和热源模型中的错误.
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