芬兰的高科技金属潜力,重点是稀土元素(REE)、钛和锂

O. Sarapaa, N. Kärkkäinen, Timo Ahtola, Thair Al-Ani
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引用次数: 5

摘要

本文根据现有数据,结合新的地球化学和矿物学、重矿物研究、地球物理测量、地质填图和最近钻探的新目标,对芬兰已知的稀土元素(REE)、Ti和Li的赋存和勘探潜力进行了评价。稀土元素的潜在岩石类型包括芬兰东部和北部的碳酸盐岩(Sokli、Korsnas)、碱性岩石(Otanmaki、Lamujarvi和Iivaara)、rapakivi花岗岩和伟晶岩(Kovela)以及含高岭土风化壳。稀土元素含量最高的是索克利碳酸盐岩杂岩的白云岩区晚期岩浆碳酸岩脉。详细的矿物学调查显示,研究区内稀土矿化类型主要为磷矿、碳酸盐矿和硅酸盐矿。矿物学和矿物化学证据表明,热液作用是研究岩石中稀土矿化的主要原因,并证实热液作用在形成过程中占主导地位。
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High-tech metal potential in Finland with emphasis on rare earth elements (REE), titanium and lithium
This article evaluates the known rare earth elements (REE), Ti and Li occurrences and exploration potential in Finland, based on existing data combined with new geochemistry and mineralogy, heavy mineral studies, geophysical measurements, geologic mapping and recent drilling of new targets. The potential rock types for REE include carbonatite (Sokli, Korsnas), alkaline rocks (Otanmaki, Lamujarvi, and Iivaara), rapakivi granite and pegmatite (Kovela), and kaolin-bearing weathering crusts in eastern and northern Finland. The highest REE concentrations occur in late magmatic carbonatite veins in the fenite area of the Sokli carbonatite complex. Detailed mineralogical investigations have revealed three distinct types of REE mineralization as phosphates, carbonates and silicates in the studied areas. Mineralogical and mineral chemical evidence demonstrates that hydrothermal processes are responsible for the REE mineralization in the studied rocks and confirms that such processes are predominant in the formatio...
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来源期刊
Central European Geology
Central European Geology Earth and Planetary Sciences-Geology
CiteScore
1.40
自引率
0.00%
发文量
8
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