在蛇形矿沉降过程中,同位素重硫的调动
Esther M Schwarzenbach1,2, Besim Dragovic3, Emmanuel A Codillo4,5
1Institute of Geological Sciences, Freie Universität Berlin, Berlin, Germany.
Science advances
|August 7, 2024
概括
原始弧形岩获得硫-34 (S) 和氧化由于板块流体. 这项研究揭示了二硫化物丰富的流体从蛇岩转移到metagabbro,解释了弧形岩的特征.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 同位素地球化学 同位素地球化学
背景情况:
- 原始弧形岩石的氧化状态和硫-34 (S) 丰富度高于中洋脊基岩石.
- 这种丰富归因于板块衍生的挥发性物质,但分类和转移机制在潜水区尚不清楚.
研究的目的:
- 为了研究在板面接口的流体透过程中的硫调动和氧化还原过程.
- 阐明硫转移的机制及其在弧形岩起源中的同位素特征.
主要方法:
- 在现场和散装岩石测量.
- 流体岩石相互作用的热力学建模.
- 来自沃尔特里山脉的横叠的蛇形岩和生态基质的metagabbro的分析.
主要成果:
- 有证据表明,硫化物占主导地位,S-丰富的流体从蛇形石转移到相邻的metagabbro.
- 观察到与流体透相关的硫调动和相关的氧化还原变化.
- 记录的流体岩石相互作用为板块接口过程提供了一个模型.
结论:
- 该研究表明,在板面接口上存在硫转移和氧化还原修饰的机制.
- 这一过程可以产生全球范围内在弧形岩中观察到的特征性氧气流动性和S签名.
- 反应板块-地幔接口岩石的融化被认为是这些弧形岩特征的来源.
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