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在流体-矿物相互作用过程中 Au-Ag 纳米熔滴的生成记录。

A track record of Au-Ag nanomelt generation during fluid-mineral interactions.

机构信息

Departament de Mineralogia, Petrologia i Geologia Aplicada, Universitat de Barcelona, Facultat de Ciències de la Terra, Barcelona, Spain.

Instituto Andaluz de Ciencias de la Tierra (CSIC-UGR), Granada, Spain.

出版信息

Sci Rep. 2023 May 16;13(1):7895. doi: 10.1038/s41598-023-35066-y.

Abstract

Recent studies have reported the significant role of Au-bearing nanoparticles in the formation of hydrothermal gold deposits. Despite the ever-increasing understanding of the genesis and stability of Au-bearing nanoparticles, it is still unknown how they behave when exposed to hydrothermal fluids. Here, we study the nanostructural evolution of Au-Ag nanoparticles hosted within Co-rich diarsenides and sulfarsenides of a natural hydrothermal deposit. We use high-resolution transmission electron microscopy to provide a singular glimpse of the complete melting sequence of Au-Ag nanoparticles exposed to the hydrothermal fluid during coupled dissolution-precipitation reactions of their host minerals. The interaction of Au-Ag nanoparticles with hydrothermal fluids at temperatures (400-500 ºC) common to most hydrothermal gold deposits may promote melting and generation of Au-Ag nanomelts. This process has important implications in noble metal remobilization and accumulation during the formation of these deposits.

摘要

最近的研究报告表明,含 Au 纳米颗粒在热液金矿床的形成中起着重要作用。尽管人们对含 Au 纳米颗粒的成因和稳定性的理解不断加深,但仍不清楚它们在暴露于热液流体时的行为如何。在这里,我们研究了天然热液矿床中富含 Co 的砷化物和硫化物中含 Au-Ag 纳米颗粒的纳米结构演化。我们使用高分辨率透射电子显微镜提供了对 Au-Ag 纳米颗粒在其宿主矿物溶解-沉淀反应过程中暴露于热液流体时完全熔化序列的独特观察。Au-Ag 纳米颗粒与热液流体的相互作用发生在大多数热液金矿床常见的温度(400-500℃)下,可能会促进 Au-Ag 纳米熔体的熔化和产生。这一过程对这些矿床形成过程中贵金属的再迁移和积累具有重要意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/992c/10188599/8d163f12f7e2/41598_2023_35066_Fig1_HTML.jpg

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