深层COHS板流体中的硫不成比例驱动了地幔 oxidation
Andrea Maffeis1, Maria Luce Frezzotti2, James Alexander Denis Connolly3
1Università di Torino, Dipartimento di Scienze della Terra, Torino, Italy.
Science advances
|March 20, 2024
概括
降温区流体从岩中释放氧化硫物种,包括硫酸盐. 这一过程发生在100公里以上的深度,显著氧化了地幔,影响了火山硫脱气.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 火山学 火山学是一门学科.
背景情况:
- 火山弧脱气硫,需要从潜水带流体中溶解的硫酸盐离子.
- 在海底深度的潜水液中,硫的确切特异性尚不清楚.
- 了解这种物种化对于模拟地幔氧化至关重要.
研究的目的:
- 为了模拟矿在碳酸盐沉积物中的溶解行为,在亚层条件下.
- 作为压力,温度和氧化还原状态的函数,确定潜水液中硫的特异化.
- 评估富含硫的液体在亚大陆地幔氧化中的作用.
主要方法:
- 电解流体热力学的应用.
- 在甲碳酸盐沉积物中模拟矿溶解.
- 在高达4.3 GPa和730°C的温度下进行模拟,考虑到法亚利特-磁铁-石英氧气缓冲器.
主要成果:
- 在亚岩层条件下的矿溶解通过不成比例地释放氧化硫物种.
- 确定的主要物种包括硫酸盐,二硫酸盐和硫化物.
- 氧化,富含硫的碳-氧--硫 (COHS) 流体的形成发生在100公里以上的深度.
- 流体组成独立于板块的氧化还原状态.
结论:
- 氧化,富含硫的COHS液体在显著深度的降温板块内产生.
- 这些流体中的硫在氧化地幔中起的作用比溶解的碳更为重要.
- 这种机制特别有效,当碳酸盐在潜水板内稳定时.
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