异常富含金属的液体形成了热水矿石矿床
Jamie J Wilkinson1, Barry Stoffell, Clara C Wilkinson
1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, Exhibition Road, London SW7 2AZ, UK. j.wilkinson@imperial.ac.uk
概括
热水矿石矿床是从富含金属的流体中形成的. 分析球石中的液体含量显示金属度明显高于以前的理解,挑战现有的矿石形成模型.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 矿物学是什么?矿物学是什么?
背景情况:
- 水热矿石沉积物是由地中的金属沉水溶液形成的.
- 传统上,酸盐/碳酸盐中的液体含量为矿石形成液体的研究提供了信息.
- 这种范式假设包含反映矿石沉解决方案.
研究的目的:
- 为了测试使用传统的流体包含用于矿石形成流体分析的范式.
- 为了研究来自-矿系统的球石内的液体含量中的金属度.
主要方法:
- 激光切除诱导合等离子体质谱法 (LA-ICP-MS). 激光切除诱导合等离子体质谱法.
- 分析来自两个不同的-矿石矿床的矿石中含有的液体含量.
主要成果:
- 球石为主体的液体内含物中的金属度比石英为主体的内含物高出两倍.
- 观察到的金属含量明显超过之前报告的值.
- 这表明矿石的形成与金属丰富的流体流入有关.
结论:
- 采用酸盐/碳酸盐托管液体内含物的传统范式可能低估了矿石液体的金属含量.
- 矿石成型系统可能涉及到高金属丰富的流体的偶尔涌入.
- 斯法莱里特托管的液体内含物提供了更准确的矿石形成液体化学表现.
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