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TitreMineralogical Signature of the St. Lawrence Columbium Mine at Oka, Québec
AuteurPercival, J B; Venance, K E; Desbarats, A J; Parsons, M B; Bilot, I; Abraham, A C; Laudadio, A B
SourceProceedings of El1: The Transport and Fate of Contaminants in the Natural Environment, GAC-MAC Annual Meeting, Kingston, May; Association géologique du Canada-Association minéralogique du Canada, Réunion annuelle, Programme et résumés vol. 40, (2017), 2017.
Année2017
Séries alt.Secteur des sciences de la Terre, Contribution externe 20160348
ÉditeurGAC-MAC
RéunionGAC-MAC Annual Meeting; Kingston; CA; mai 14-18, 2017
Documentlivre
Lang.anglais
Mediapapier; en ligne; numérique
Formatspdf
ProvinceQuébec
Sujetscarbonatites; roches hyperalumineuses; niobium; gisements minéraux; niocalite; latrappite; pyrochlore; analyses géochimiques; analyses minéralogiques; élimination des résidus; résidus; géochimie des résidus; géochimie; minéraux métalliques; minéraux radioactifs
ProgrammeOutils d'adaptation et d'impacts sur l'environnement pour les mines de métaux, Géosciences de l'environnement
LiensOnline - En ligne
Résumé(disponible en anglais seulement)
Global demand for modern technology has increased the requirement for critical metals including rare earth elements (REE), platinum-group elements, niobium, tantalum, indium and tungsten. These elements are used in components in high tech devices, and in development of green and defence technologies. In Canada, the supply of these elements is limited to a few deposits that are currently being mined (Niobec (Nb), St. Honoré, QC ) or under development (e.g., Aley (Nb) in B.C.; Nechalacho-Thor Lake (Nb, Ta, HREE) in NT; Hoidas Lake (Nd) in SK; Eldor (Nb, Ta, REE), Kipawa (HREE), Montviel (REE), and Strange Lake (HREE) in QC). These deposits commonly occur in carbonatite or peralkaline granite rocks, have complex mineralogy, and are associated with the radioactive elements U and Th.
To better understand the potential effects from mining REE and other critical metal deposits, a study was initiated at the GSC as part of the Environmental Geoscience Program aimed at determining risks from metal mining. The St. Lawrence Columbium Mine in Oka, QC, formerly one of the largest Nb producers in the world, afforded a good proxy to examine long-term environmental effects. This open pit and underground mine operated between 1961 and 1977 and produced 3,536,200 tonnes of Nb-bearing ore (average grade 0.51% Nb2O5) and 3,857,350 t of waste material. Annual production of concentrates containing ~ 52% Nb2O5 was ramped up to 2.25 million kg from 113,000 kg in the early seventies (Gold et al., 1986). The Oka site is composed of a carbonatite and alkaline rock complex contemporaneous with the Monteregion Hills. Over 70 minerals have been identified and this complex is the type locality for two minerals (niocalite and latrappite). The complex is formed largely of silica-undersaturated rocks of the melilitite and nepehelinite series. Niobium occurs in pyrochlore group minerals in sövite, a calcite-bearing carbonatite.
This study focusses on the geochemical and mineralogical controls of metal mobility. To this end, representative rock samples, tailings, and waters from the open pits, tailings, decant pond and local creeks are being analysed. Representative rock samples were collected from large waste rock piles and tailings samples were collected from two sites at 5 and 30 cm depths each. Preliminary mineralogical analyses by XRD show tailings are rich in calcite (~90 wt%) with minor to trace amounts of apatite, niocalite, perovskite and pyrochlore. Rock samples contain abundant calcite with variable amounts of gypsum, apatite, mica (biotite/phlogopite), chlorite, amphibole, garnet, pyroxene and zeolite group minerals. Some samples contained sufficient pyrochlore to be detectable in a calcite-rich sample. Slag material in the central area of the mine site is dominated by high-temperature hibonite and grossite along with vesuvianite, as well as minor amounts of augelite, bredigite, cristobalite, perovskite, thorite and uraninite (not in order of abundance) interspersed in a glass matrix. The concern from this site is the radioactivity of thorium and uranium and their possible mobility along with other critical metals. The mineralogical footprint of this site is complex and its characterization will aid in determining the mineralogical and geochemical controls of the contaminants. Lessons from Oka will be applied to deposits currently under development.
Résumé(Résumé en langage clair et simple, non publié)
Signature minéralogique de la mine de niobium St. Lawrence d¿Oka, au Québec. Le présent document porte sur les résultats minéralogiques préliminaires de travaux réalisés sur le terrain à la mine St. Lawrence, en 2015 et en 2016. Le site visé est une partie du programme « Géoscience environnementale », qui a pour objet, entre autre, les risques environnementaux posés par l¿exploitation de mines de métaux. Il constitue un analogue idéal de gisements similaires mis en valeur pour en extraire des éléments des terres rares et/ou des métaux essentiels. Il est important de connaître la signature minéralogique de la mine St. Lawrence pour en produire un ou des modèles géochimiques et en évaluer les risques de déplacement des contaminants, dont ceux présentant une radioactivité inhérente.
GEOSCAN ID299710