Mineralogy and Beneficiation of Lamujärvi Syenites
- 1 Geological Survey of Finland, GTK Mintec, Outokumpu, Finland
- 2 Geological Survey of Finland, GTK Mintec, Outokumpu, Finland
- 3 Geological Survey of Finland, Kuopio, Finland
- 4 Geological Survey of Finland, GTK Mintec, Outokumpu, Finland
Abstract
The Lamuj ä rvi syenites intrusions occur within Svecofennian (ca. 1.92 Ga) gneisses, ca. 70 km west of the Otanmaki alkaline area in central Finland. Previous studies have revealed zones in the syenites that display strong enrichment in Zr (1587 ppm), Nb (up to 685 ppm), Ta (up to 82 ppm), and REE (up to 5350 ppm). The major REE-bearing minerals in the Lamujarvi syenites are allanite and monazite. A sample of the Lamuj ä rvi syenites with the REE content of 4700 ppm was studied on the mineralogy and beneficiation at GTK Mintec. The mineralogical analysis was conducted by MLA. The REE-bearing minerals allanite, parisite, zircon, and apatite were identified at significant concentrations and high contents of titanite (15.4%), biotite (30.9%) and magnetite (8.2%) were displayed in the sample. The beneficiation experiments by flotation, wet low and high gradient magnetic separations and gravity separation with a shaking table were carried out. A composite REE-Ti concentrate with REE 23,000 ppm, Zr 5000 ppm, Nb 3400 ppm and TiO2 25.5% at REE and Ti recoveries of 57% and 54% was obtained. In addition, biotite and magnetite concentrates were gained as by-products.
- Goodenough, K.M., et al. (2016) Europe’s Rare Earth Element Resource Potential: An Overview of REE Metallogenetic Provinces and Their Geodynamic Setting. Ore Geology Reviews, 72, 838-856. http://dx.doi.org/10.1016/j.oregeorev.2015.09.019
- Sarapää, O. and Sarala, P. (2013) Rare Earth Element and Gold Exploration in Glaciated Terrain—Example from the Mäkärä Area, Northern Finland. Geochemistry: Exploration, Environment, Analysis, 13, 131-143. http://dx.doi.org/10.1144/geochem2012-136
- Arzamastsev, A., et al. (2008) The Khibina and Lovozero Alkaline Massifs: Geology and Unique Mineralization. 33 IGC Excursion No. 47, Apatity, 22 July-2 August 2008, 1-58.
- Zaitsev, A.N., et al. (2014) Rare-Earth Elements Minerals in Carbonatites of the Kola Alkaline Province (Northern Fennoscandia). 1st European Rare Earth Resources Conference, Milos Island, 4-7 September 2014, 343-347.
- Al Ani, T. and Sarapää, O. (2013) Geochemistry and Mineral Phases of REE in Jammi Carbonatite Veins and Fenites, Southern End of the Sokli Complex, NE Finland. Geochemistry: Exploration, Environment, Analysis, 13, 217-224. http://dx.doi.org/10.1144/geochem2011-088
- Vartiainen, H. (1980) The Petrography, Mineralogy and Petrochemistry of the Sokli Carbonatite Massif, Northern Finland. Geological Survey of Finland, Bulletin 313, 126.
- Sarapää, O., et al. (2013) Rare Earth Exploration Potential in Finland. Journal of Geochemical Exploration, 133, 25-41. http://dx.doi.org/10.1016/j.gexplo.2013.05.003
- Fandrich, R., et al. (2007) Modern SEM-Based Mineral Liberation Analysis. International Journal of Mineral Processing, 84, 310-320. http://dx.doi.org/10.1016/j.minpro.2006.07.018
- Gu, Y. (2003) Automated Scanning Electron Microscope Based Mineral Liberation Analysis An Introduction to JKMRC/FEI Mineral Liberation Analyser. Journal of Minerals & Materials Characterization & Engineering, 2, 33-41. http://dx.doi.org/10.4236/jmmce.2003.21003
- Zeh, A. (2004) Crystal Size Distribution (CSD) and Textural Evolution of Accessory Apatite, Titanite and Allanite during Four Stages of Metamorphism: An Example from the Moine Supergroup. Scotland. Journal of Petrology, 45, 2101-2132. http://dx.doi.org/10.1093/petrology/egh049