一个用于超湿弧形岩石的石盒
Chetan Nathwani1,2, Jon Blundy3, Simon J E Large4
1Department of Earth and Planetary Sciences, ETH Zürich, Zürich, Switzerland. chetan.nathwani@eaps.ethz.ch.
Nature communications
|October 17, 2024
概括
超湿的岩石,含水量高,结晶和低. 这一发现表明,超湿的岩是常见的,对于形成大型铜沉积物至关重要.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 经济地质学 地质学
背景情况:
- 弧形岩通常含有2-6%的H2O.
- 有证据表明,一些深弧岩是"超湿"的 (>6重量%H2O).
- 在岩分化的过程中,的行为对融化水的含量敏感.
研究的目的:
- 为了研究融水含量对在岩石分化过程中的 behavior的影响.
- 为了确定氧化的度是否可以表明存在超湿的存在.
- 评估超湿岩在矿铜沉积物形成中的作用.
主要方法:
- 磁性系统的热力学建模.
- 分析氧化的度.
- 地质化学研究与矿铜沉积物相关的岩系统.
主要成果:
- 超湿的 magma 结晶了低,均度 (<10 ppm) 的.
- 这是由于缩的和温度下降而增加化的H2O而发生的.
- 子的度显示,在Río Blanco-Los Bronces铜沉积形成之前,过渡到超湿的岩层.
结论:
- 超湿岩比以前认为的更为普遍.
- 低,均的氧化度是超湿岩的关键指标.
- 超湿的岩在矿铜沉积物的起源中起着根本性的作用.
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