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TitleColumbite-tantalite and pyrochlore as indicator minerals for specialty metal deposits
AuthorMackay, D A R; Simandl, G J
SourceBritish Columbia Geological Survey, Geofile no. 2014-07, 2014 p. 1
Year2014
Alt SeriesEarth Sciences Sector, Contribution Series 20120508
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceBritish Columbia
NTS83D/03; 93J/09; 93N/09; 94B/05
AreaAley; Lonnie; Wicheeda; Blue River
Lat/Long WENS-119.5000 -119.0000 52.2500 52.0000
Lat/Long WENS-122.5000 -122.0000 54.7500 54.5000
Lat/Long WENS-124.5000 -124.0000 55.7500 55.5000
Lat/Long WENS-123.5000 -123.5000 56.5000 56.2500
Subjectsgeochemistry; minerals; indicator elements; mineral exploration; mineral deposits; pegmatites
Illustrationsgraphs; photomicrographs; location maps
ProgramRare-Metal Ore Systems, Targeted Geoscience Initiative (TGI-4)
AbstractColumbite-tantalite series and pyrochlore supergroup (betafite, microlite, and pyrochlore groups) minerals are the main constituents of Ta and Nb ores. They are present in carbonatites, pegmatites, peralkaline intrusions, Li, REE, Be, Zr, W, Sn, and Cs-bearing deposits associated with granitoids, in saprolites overlying these deposits, in associated stream and lake sediments, and till. Based on Ta/ Nb+Ta) and Mn/(Mn+Fe) atomic ratios, members of the columbite-tantalite series [(Fe,Mn)Nb O and (Fe,Mn)Ta O respectively; can be divided into tantalite-(Fe), columbite-(Fe), columbite- (Mn), and tantalite-(Mn). Li-Nb-Ta-REE-Sn enriched (specialty metal) granites are known to contain predominantly columbite-(Fe) with Mn/(Mn+Fe) atomic ratio > 0.1, columbite- (Mn), and tantalite-(Mn). Pegmatite-related deposits are known to contain tapiolite [tetragonal equivalent of tantalite-(Fe)], all major varieties of tantalite, and Ta-rich end members of columbite. There is a paucity of columbite analyses from carbonatite-hosted deposits; however, preliminary compilation suggests that they contain Nb-rich columbite-(Fe) with Mn/(Mn+Fe) atomic ratio <= 0.15. Pyrochlore supergroup minerals are present in the same deposits as columbitetantalite minerals. Betafite [(Ca,U) (Ti,Nb,Ta) O (OH)] is common in pegmatites and present in some carbonatites. Microlite [(Na,Ca) Ta O (O,OH,F)] is found predominantly in rare element pegmatites and in miarolitic cavities in granites. Pyrochlore [(Na,Ca) Nb O (OH,F)] is characteristic of carbonatites, but is also present in other alkaline rocks. Discrimination diagrams based on composition of columbitetantalite and/or pyrochlore minerals may allow exploration geologists to relate indicator mineral chemistry to established specialty metal deposit models. For example, Nbrich pyrochlore and columbite-(Fe) with Mn/Mn+Fe atomic ratio <= 0.15 are expected in carbonatite-related specialty metal deposits, while tapiolite, microlite, and Ta-rich betafite are characteristic of pegmatite-related mineralisation.
GEOSCAN ID296088