通过沉积物沉降,低效地将气运送到下层地幔
Weihua Huang1, Yan Yang2, Yuan Li3,4
1Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province, School of Earth Sciences, Zhejiang University, Hangzhou, China.
Nature communications
|August 14, 2024
概括
在岩到K-荷兰石过渡期间,研究了沉积物中的引. 凯荷兰保留的比预期的要少,这表明板块沉积物对地球深层的贡献很小.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
背景情况:
- 了解地球深层的源需要在沉积过程中追踪沉积.
- 石到K-荷兰石的过渡是压板块的一个关键过程.
研究的目的:
- 为了研究岩沉积物的气行为,跨越岩-K-荷兰岩过渡.
- 在高压和高温下量化矿物质和流体之间的分区.
主要方法:
- 高压和高温实验模拟了俯冲条件 (10-12 GPa,800-1100 °C).
- 在石-流体和K-荷兰石-流体系统中分析分区系数.
主要成果:
- 石的稳定性由 (NH4+) 增强.
- 分成K-荷兰是压力依赖和温度依赖的,在温暖的地热沿线的保留率较低.
- K-荷兰仅保留了基的约43% (冷地热) 和约26% (热地热).
结论:
- 石沉积物最多每年为下层地幔贡献约1.5×10^8公斤的.
- 岩石沉积物可能占下层地幔气预算的不到15%.
- 大多数下层地幔气很可能是原始起源的.
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