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Updated: Jul 8, 2025

Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
岩石不混合性和磁铁沉积物的起源
Dorota K Pietruszka1, John M Hanchar2, Fernando Tornos1,3
1Department of Earth Sciences, Memorial University of Newfoundland, St. John's, NL, A1B 3X5, Canada.
磁石-酸铁沉积物的起源仍在争论中. 在智利埃尔拉科 (El Laco) 发现的融沉积物的新研究表明,这些沉积物是由富含铁的融形成的,为它们的形成提供了洞察力.
科学领域:
- 经济地质学 地质学
- 伊格尼岩石学 伊格尼岩石学
- 矿产矿产储备矿产储备矿产储备矿产储备矿产储备矿产储备矿产储备矿产储备
背景情况:
- 磁石-酸铁 (MtAp) 沉积物的起源是有争议的,有争议的水热或岩起源.
- 了解MtAp矿床的起源对于全球铁矿石勘探至关重要.
研究的目的:
- 为了调查智利El Laco MtAp矿床的石化过程.
- 为融化演化过程提供直接证据,从而导致MtAp矿化.
主要方法:
- 分析融的含有物被困在来自El Laco石矿的石质晶体中.
- 微热度计和化学分析融含量含量.
主要成果:
- 融的入揭示了融不混合性的证据,将富含Si的融和富含Fe的融分开.
- 富含铁的融物中含有硫化物,酸盐和富含C-O-HFSE的残留物,在1145°C化.
- 这表明了酸盐和富含Fe-P的融物之间的联系,这些融物负责磁铁的形成.
结论:
- 埃尔拉科矿化源于富含Fe-P的融物的结晶.
- 这一发现支持了MtAp沉积形成的岩模型.
- 为了解全球类似的铁矿石矿床提供了一个框架.
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