在Maoniuping碳酸盐中发生反应驱动的岩结晶
1State Key Laboratory of Deep Earth and Mineral Exploration, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, PR China. ly@cags.ac.cn.
毛尼乌平稀土元素 (REE) 沉积物是从碳酸盐融的碳酸盐盐中形成的,而不是热水流体. 宿主岩石元素的同化导致了固化,这可能是其他碳酸盐宿主REE沉积物中常见的过程.
科学领域:
- 地质地质地质地质地质地
- 经济地质学 地质学
- 石化学 石化学是一门学科.
背景情况:
- 火性岩石是由岩固化形成的,对于矿产沉积物而言,经常提出水热变化.
- 马云平稀土元素 (REE) 矿床的起源被归因于热水过程,但缺乏直接证据.
- 了解REE矿床的起源对于全球资源管理至关重要.
研究的目的:
- 为了研究Maoniuping REE矿床的形成机制.
- 确定岩与热水过程在REE矿化中的作用.
- 为了阐明碳酸盐融的固化过程与宿主岩石相互作用的关系.
主要方法:
- 来自Maoniuping矿床的岩石样本进行了详细的纹理和化学分析.
- 显微镜检查以确定矿物质组合和相互作用.
- 地质化学研究融化主体岩石相互作用和元素同化.
主要成果:
- 毛尼乌平的REE矿床起源于盐融的岩石碳酸盐,而不是热水流体.
- 碳酸盐和石英锡尼特宿主之间的相互作用产生了化.
- 结合的转基体导致了污染,通过耐火酸盐 (抗肉质) 的结晶和Na和K的去除导致了融化固化.
结论:
- 碳酸盐化物可以通过从环境中吸收元素来固化,这一过程与简单的冷却或挥发性溶解不同.
- 由结合的抗肉化和化驱动的固化影响矿物质组合和矿石结构.
- 这种火性形成过程可能对全球许多碳酸盐托管的REE沉积物具有重要意义.
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