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TitleWhy is the Proterozoic Athabasca Basin endowed with rich and large unconformity-related uranium deposits?
 
AuthorChi, G; Potter, E GORCID logo; Rabiei, M; Wang, Y
SourceSEG 100 Conference, abstract volume; 2021 p. 1
Image
Year2021
Alt SeriesNatural Resources Canada, Contribution Series 20210206
PublisherSociety of Economic Geologists
MeetingSEG 100 Conference; Whistler; CA; September 14-17, 2021
Documentbook
Lang.English
Mediapaper
ProvinceSaskatchewan
NTS74
Lat/Long WENS-112.0000 -104.0000 60.0000 56.0000
Subjectseconomic geology; Science and Technology; uranium; uranium deposits; unconformities; unconformity-type deposit; Athabasca Basin; Proterozoic
ProgramTargeted Geoscience Initiative (TGI-5) Uranium ore systems - fluid pathways
Released2021 09 14
AbstractThe Proterozoic Athabasca Basin in northern Canada hosts a number of high-grade (mostly >1%, some >10% U) and large-tonnage uranium deposits, making Canada the second largest producer of uranium in the world. These deposits are mostly located near the basal unconformity between the basin and crystalline basement and are termed unconformity-related uranium (URU) deposits. The deposits are spatially associated with reactivated basement faults and hydrothermal alteration halos characterized by chlorite, tourmaline, kaolinite and illite. They are generally interpreted to have resulted from reaction between oxidizing, uranium-bearing, basin-derived brines and reducing lithologies in, or reducing fluids derived from, the basement. Although this "diagenetic-hydrothermal" model adequately describes formation processes and conditions of the URU deposits, it does not explain why the Athabasca Basin is exceptionally endowed in uranium mineralization; indeed, although URU deposits occur elsewhere in the world, few of them (e.g. Kombolgie Basin in Australia) are comparable to those in the Athabasca Basin. Chemical analyses of fluid inclusions in quartz overgrowths in sandstones of the Athabasca Basin, and drusy quartz in both mineralized and barren areas along structures hosting URU deposits, suggest basin-wide development of uranium-rich brines. Such unusual, large-scale formation of uranium-rich brines, which is possibly the critical reason for the rich endowment of uranium deposits in this basin, may be attributed to several geological factors. First, the basin is flanked by two orogens, the Taltson Magmatic Zone - Thelon Orogen to the west and the Trans-Hudson Orogen to the east; both of which contain large amounts of granitic rocks that may have provided abundant uranium-rich detritus to the basin. Second, the low mud content of the sandstones, related in part to the lack of land vegetation in the Proterozoic, enhanced fluid circulation. Third, increased atmospheric oxygen levels in the late Paleoproterozoic, as recorded by the red beds in the basin, enhanced extraction of uranium from the sediments. Fourth, basinal brines derived from seawater evaporation, as indicated by evaporitic carbonate rocks above the sandstones and high-salinity fluid inclusions in quartz overgrowths, increased uranium extraction. Finally, elevated temperatures, as recorded by fluid inclusions, clay geothermometry and zircon thermochronology, facilitated fluid convection and uranium extraction. Fluid convection is reflected by basin-scale quartz precipitation - dissolution patterns and demonstrated by reactive mass transport modeling. The elevated temperatures may be related to high radiogenic heat-producing felsic intrusions at depth or upwelling of the asthenosphere in relation to the break-up of the Nuna supercontinent. Based on regional geological and geochronological data, we propose that that these conditions came together in the Athabasca Basin at ca. 1550 Ma, which, together with reactivation of basement-rooted structural zones channelling deep-sourced reducing fluids toward the unconformity, resulted in large-scale URU mineralization. Although individual factors may be satisfied in many other basins, the combination of them all is rare. Therefore, the unusually rich uranium deposits in the Athabasca Basin are the result of coupling of multiple favorable geological factors, including both shallow (basinal) and deep (thermo-tectonic) processes, at a specific time and location in the Earth's crust.
Summary(Plain Language Summary, not published)
The Targeted Geoscience Initiative (TGI) is a collaborative federal geoscience program that provides industry with the next generation of geoscience knowledge and innovative techniques to better detect buried mineral deposits, thereby reducing some of the risks of exploration. This contribution summarizes current hypotheses on why the ore grades and tonnages of the Athabasca Basin uranium deposits are far greater than global analogues: the coupling of multiple favorable geological factors, including both shallow (basinal) and deep (thermo-tectonic) processes, at a specific time and location in the Earth's crust.
GEOSCAN ID328696

 
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