在水热矿石系统中运输过渡性不溶性贵金属
Néstor Cano1,2, José M González-Jiménez3, Antoni Camprubí4,5
1Instituto de Geología, Universidad Nacional Autónoma de México (UNAM). Ciudad Universitaria, 04510, Coyoacán, CDMX, Mexico. nacanoh@geologia.unam.mx.
Nature communications
|March 14, 2025
概括
热水流体可以悬浮和运输微小的富含金属的化物,帮助贵金属 (金,银) 矿石的形成. 这一发现揭示了在地质系统中金属运输和沉积的新机制.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 矿物物理 矿物物理
背景情况:
- 在热水系统中,贵金属的运输传统上涉及复杂化连接体.
- 在这些流体中,金属丰富的融体的作用和物理运输仍然不太清楚.
- 关于融化流体相互作用的证据对于理解矿石起源至关重要.
研究的目的:
- 调查和带介导的传输机制的共存和相互作用.
- 为了确定富含金属的化物是否可以通过热水流体进行物理运输.
- 阐明融运输在贵金属矿化中的作用.
主要方法:
- 在表热流体 (<400°C) 中观察纳米到微米大小的聚矿物质含.
- 纳入成分 (Ag-Au-Cu-Pb-As-Sb-S-Se) 的分析.
- 粒子流化和沉理论的数值建模.
主要成果:
- 有证据表明,硫化硫盐溶液在表热液体内以悬浮形式运输.
- 在冷却后形成不规则的,类似斑块的聚矿物质含 (5nm至40μm).
- 热水流体可以在流速<10−1 m/s时机械运输纳米微融物.
结论:
- 热水流体在物理上运输富含金属的纳米微融体,补充了连接体运输.
- 纳米化前体的凝聚可能发生在运输过程中,影响矿化.
- 这种融化运输机制对于理解贵金属矿石的形成具有重要意义.
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