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Tehery-Wager Geoscience Project: Findings from the 2015 bedrock mapping campaign Holly Steenkamp, Canada-Nunavut Geoscience Office Natasha Wodicka, Geological Survey of Canada Christopher Lawley, Geological Survey of Canada Tony Peterson, Geological Survey of Canada Carl Guilmette, Université Laval The Tehery-Wager Project Regional geoscience initiative: • Targeted bedrock mapping • Surficial geology mapping • Targeted stream sediment surveys Collaborative project: • Geological Survey of Canada (GEM 2 - South Rae Activity) • Canada-Nunavut Geoscience Office (SINED) Contributions from: • Université Laval • Dalhousie University • University of Victoria • University of New Brunswick • Université du Québec à Montréal • Nunavut Arctic College Duration: • 2 field seasons (2015/2016), outputs through 2̴ 019 Project Location Davis Strait Hudson Bay Mapping prior to 2015… • Reconnaissance mapping • Wright, 1955 • Lord and Wright, 1967 • Heywood, 1967 • Gordon and Heywood, 1988 Daly Bay complex • Henderson et al., 1990 Wager Shear Zone • Panagapko et al., 2003 – RPM • New reconnaissance survey by the GSC in 2012 • McMartin et al., 2013 • Wodicka et al., in prep Project Objectives 1) Characterize and define distinct units within the Archean gneiss • Define their relationships with overlying supracrustal rocks • Snow Island suite K-feldspar porphyritic monzogranite? 2) Document stratigraphy of supracrustal belts, determine depositional ages and environments • Correlations to other known sequences? 3) Determine the timing, extent and degree of metamorphism and deformation in the area related to the Snowbird Tectonic Zone and/or terminal collision of the Trans-Hudson Orogeny • • Peak pressure/temperature of metamorphism, spatial distribution Development of trans-lithospheric fault systems 4) Evaluate the economic potential of the area • • Metal and carving stone potential? Diamond potential? Do large-scale faults provide favourable environments for mineralization? 2015 Field Season • • • • • June 30 – Aug 2 14 field crew 5 camp crew 1 Bell 206 LR Turbo Otter supply runs 2015 Mapping Archean Tonalite to Granodiorite • Biotite ± hornblende • Granitic injections that cut foliation and are subsequently deformed • Pods, lenses, rafts of mafic rocks (e.g. pyroxenite, diorite) and supracrustal rocks (e.g. amphibolite, calcsilicate) • Van Breemen et al., 2007: U-Pb zircon crystallization ages 2699 ± 11 Ma, 2701 ± 14 Ma • Compositional complexity and variability – likely more phases to identify Archean Monzo- to Syenogranite • • • • • Contains biotite, magnetite, rare muscovite Foliation defined by biotite, compositional layering Cut by syenite dykelets that are subsequently transposed Nature of contact with Archean tonalite-granodiorite is poorly exposed Unknown age K-Feldspar Porphyritic Monzogranite K-Feldspar Monzogranite Tonalite • Rapakivi texture, coeval gabbro/diorite phases • Similar characteristics to felsic plutonic rocks of the 2.6 Ga Snow Island suite • Mylonitic zone at contact to underlying orthogneiss Supracrustal Rocks • Occur as panels between layers of Archean orthogneiss • Granulite-facies mineral assemblages with partial retrogression to amphibolite-facies phases • Include: • Sill-Bt quartzite (3.7-2.55 Ga detritus – Ferderber et al., 2013) • Grt-Bt±Sill±melt semipelite with local psammite and pelite layers • Grt-Cpx amphibolite Supracrustal Rocks • Includes: • • • • • Garnetite Iron formation Ultramafic boudins Calcsilicate Rare marble Ultrapotassic Intrusions • Zoned, bimodal intrusions with magma mixing textures • Well exposed plutonic bodies, only 1 minette dyke identified • Correlative with Christopher Island formation and Martel syenite? Cpx-Bt Syenite Cpx Monzonite Phlg Clinopyroxenite Undeformed Granitic Rocks • • • • • Monzogranite to syenogranite dykes and sills Homogeneous texture and mineralogy Rare fluorite Contain xenoliths of orthogneiss and paragneiss Possibly correlative with felsic rocks of the 1.85-1.81 Ga Hudson suite Economic Considerations • Stream sediment and till sample findings of McMartin et al. (2013) highlight locations for follow-up work: • Gossanous metasedimentary rocks – anomalous Ag, Au, Bi, Cu and presence of safflorite • Ultrapotassic intrusions – REE potential in most fractionated parts of the plutons • Diamond potential • Nanuq property (Peregrine Diamonds) • Carving stone Thank you! • Hamlet of Chesterfield Inlet • Hudson Bay Helicopters • Ookpik Aviation • Polar Continental Shelf Program • Discovery Mining Also See: Wodicka et al., 2015 – GSC Open File 7970, 2015 field report McMartin et al., 2015 – Poster Session at Arena – 2015 Surficial mapping Coming Soon – Steenkamp et al., 2015 – CNGO Summary of Activities report