40K-(40) Ar限制了回收大陆地到地幔中的限制
1Laboratoire des Sciences de la Terre, Ecole Normale Superieure, 69364 Lyon cedex 7, France.
概括
和在岩提取和排气过程中的行为会影响地的组成. 有限的地-地幔交换意味着深层地幔的过程主要塑造了上层地幔的化学结构.
科学领域:
- 地质化学 地质化学
- 地质地质地质地质地质地
- 地球科学 地球科学 地球科学
背景情况:
- 地球地和大气中的 (K) 和 (Ar) 储量与地质过程有关.
- 了解地-地幔相互作用对于破译行星进化至关重要.
研究的目的:
- 为了限制地和大气中的相对数量.
- 评估大陆地的沉降程度及其对地幔构成的影响.
主要方法:
- 分析K提取到岩石中的情况.
- 在化过程中Ar脱气的建模.
- 地质化学建模地-地幔物质交换.
主要成果:
- 的提取和融期间的气排放显著影响地的K和大气中的Ar预算.
- 在地球历史上,不到30%的大陆地质量被入地幔.
- 沉积沉积物的很大一部分 (50-70%) 被回收到深层大陆地中.
结论:
- 大陆地和上层地幔之间的有限交换表明,深层地幔过程是上层地幔化学的主要驱动因素.
- 上层地幔的长期化学进化更多地受到深层地幔水库的影响,而不是地回收.
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