结合的解和极端分化是产生丰富的巨型金矿石的关键
Hai-Zhen Wei1,2,3, Martin R Palmer4, Zhiqin Xu1,2
1State Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, People's Republic of China.
概括
这项研究揭示了矿沉积物中丰富的三阶段模型,涉及深度解氧,岩分化和液体溶解. 这有助于我们更好地了解这些经济重要地质构成中的稀有金属度.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 石化学 石化学是一门学科.
背景情况:
- 结石沉积物在经济上具有重要意义,但它们的形成过程仍在争论中.
- 提出的关键机制包括极端的岩分化和沉积岩的直接解体.
研究的目的:
- 通过使用两个主要的拟议过程,量化建模矿中的丰富.
- 为了调查贾吉卡皮格马矿场,这是一个主要的全球资源.
主要方法:
- 用地化学建模来模拟丰富的情况.
- 进行了一项---- (Li-Si-B-Ba) 同位素研究.
- 从深度钻孔和区域形岩突出的系统采样提供了数据.
主要成果:
- 提出了三阶段的石场形成模型.
- 第一个阶段:通过与变态流体的深度解体产生稀有金属丰富的化物.
- 第二阶段:持续的岩分化导致稀有金属的丰富.
- 第三阶段:由于过压和延伸应力,富含水量的矿物质从富含水的岩中逃逸.
结论:
- 拟议的模型整合了度的anatexis和差异化.
- 了解这些过程有助于定位矿中的资源的勘探.
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