A reappraisal of the Nonacho Basin (Northwest Territories, Canada): Record of post-orogenic collapse and marine flooding in the Palaeoproterozoic of the Rae Craton

Three Orosirian basins and associated foreland thrust-fold belts are preserved on the margins of Slave craton. All three are related to orogenic belts where oceans opened and later closed uniting new crustal partners. Great Slave basin differs from Kilhigok and Coronation basins in ways that have defied explanation. It lacks a passive-margin sequence and hosts two discrete igneous suites, separated by large-scale thrusting, occurring well after the adjacent paleocean had closed. Here we report U-Pb zircon geochronology by CA-ID-TIMS for a member of each suite to constrain the age and origin of post-collisional thrusting. A widespread pulse of mainly phreatic alkaline volcanism, coeval with renewed foredeep flexure, occurred at 1889.0±0.7 Ma (2σ internal error). A quartz-monzodiorite body, one of a belt-parallel chain of laccoliths that postdate thrusting, was emplaced at 1866.9±0.9 Ma. These ages bracket renewed foredeep sedimentation and thrusting that telescoped major facies zones and was rooted within the basin. The older age is 70 and 30−60 Myr younger than collision in Thelon and Taltson orogen, respectively. We attribute post-collisional thrusting and foredeep subsidence to ‘eduction’—the upward and outward ejection of partly-subducted crust—and postulate that the top of the ejected wedge was a normal-sense detachment fault projecting beneath Nonacho basin. We infer that eduction was triggered by slab failure, producing alkaline volcanism, and ended with delamination and laccolith emplacement. Eduction was facilitated by tradewind–driven erosion. Delamination was enabled by crustal transfer to the educted wedge, reducing footwall buoyancy. Slab-failure and/or delamination removed the passive margin.

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Public geoscience solutions for diversifying Canada's critical mineral production

Gadd

Lawley

Corriveau

et al. 2022

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Achieving net-zero carbon emissions goals will increasingly rely on critical mineral resources while simultaneously decreasing the extraction, processing and use of hydrocarbons as the primary provider of energy. Canada is well-positioned to contribute to this effort through a series of innovative policy and research initiatives, and it is Canada's goal to be a stable supplier of critical minerals into the future. To this end, Natural Resources Canada and the Geological Survey of Canada invest financial resources into critical mineral research initiatives. This research aims to generate precompetitive baseline geological, geochemical and geophysical data for large, underexplored regions within Canada, whereas targeted studies focus on mineral systems science and improved exploration models for the large variety of critical mineral resources distributed throughout Canada. These research approaches can be combined, digitally, to generate mineral potential models. These ongoing efforts by the Geological Survey of Canada enhance the viability of Canada being (or maintaining its status as) a hub for critical mineral resource development and processing well into the future.

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A reappraisal of the Nonacho Basin (Northwest Territories, Canada): Record of post-orogenic collapse and marine flooding in the Palaeoproterozoic of the Rae Craton

Cited by 4 publications

References 121 publications

Tectonic evolution of the South Tazin Lake shear zone; a major Arrowsmith-age (ca. 2.36 Ga) structure in the SW Rae craton, Laurentia

Tectonic evolution of the South Tazin Lake shear zone; a major Arrowsmith-age (ca. 2.36 Ga) structure in the SW Rae craton, Laurentia

Crustal eduction and slab-failure magmatism in an Orosirian (2.05–1.80 Ga) postcollisional cratonic foredeep: geochronology of Seton volcanics and Compton laccoliths, Tu Cho (Great Slave Lake), NWT, Canada

Public geoscience solutions for diversifying Canada's critical mineral production

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