Released Dataset Petrography, quantitative mineralogy, and U-Pb geo- chronology of the Boundary Zone Zn-Pb ± Ag deposit, Yukon, Canada Cite as: Copy citation to clipboard Grema, Haruna M.; Wudarska, Alicja; Wilke, Franziska D. H.; Schleicher, Anja M.; Milton, Jack E.; Magnall, Joseph M.; Gleeson, Sarah A.; Schulz, Hans-Martin (2024): Petrography, quantitative mineralogy, and U-Pb geo- chronology of the Boundary Zone Zn-Pb ± Ag deposit, Yukon, Canada. GFZ Data Services. https://doi.org/10.5880/GFZ.3.1.2024.007 Status I N R E V I E W : Grema, Haruna M.; Wudarska, Alicja; Wilke, Franziska D. H.; Schleicher, Anja M.; Milton, Jack E.; Magnall, Joseph M.; Gleeson, Sarah A.; Schulz, Hans-Martin (2024): Petrography, quantitative mineralogy, and U-Pb geo- chronology of the Boundary Zone Zn-Pb ± Ag deposit, Yukon, Canada. GFZ Data Services. https://doi.org/10.5880/GFZ.3.1.2024.007
Abstract The Boundary Zone prospect (Yukon, Canada) is a Zn-Pb-Ag prospect hosted by siliciclastic rocks in the Macmillan Pass district. The main host units comprise the Late Ordovician to Early Silurian Duo Lake Formation and the Middle to Late Devonian Portrait Lake Formation. Sulfide mineralization is hosted in mudstones, conglomerates, diamictites, and volcaniclastic rocks, with stratabound, vein, and breccia-hosted sulfides consisting of sphalerite, pyrite, galena, with minor chalcopyrite and sulfosalts.
This data publication comprises results of analyses conducted on drill core samples obtained from the Boundary Zone. The data originates from multi-scale petrographic examination, quantitative X-ray diffraction (QXRD), electron probe microanalysis (EPMA), and secondary ion mass spectrometry (SIMS) U-Pb fluorapatite geochronology. All the analyses were caried out at the GFZ German Research Centre for Geosciences, Potsdam, Germany.
Authors Grema, Haruna M. ;GFZ German Research Centre for Geosciences, Potsdam, Germany;Institute of Geological Sciences, Freie Universität Berlin, Berlin, GermanyWudarska, Alicja ;GFZ German Research Centre for Geosciences, Potsdam, Germany;Institute of Geological Sciences, Polish Academy of Sciences, Warsaw, PolandWilke, Franziska D. H. ;GFZ German Research Centre for Geosciences, Potsdam, GermanySchleicher, Anja M. ;GFZ German Research Centre for Geosciences, Potsdam, GermanyMilton, Jack E.;Fireweed Metals Corporation, British Columbia, Canada Magnall, Joseph M. ;GFZ German Research Centre for Geosciences, Potsdam, GermanyGleeson, Sarah A. ;GFZ German Research Centre for Geosciences, Potsdam, Germany;Institute of Geological Sciences, Freie Universität Berlin, Berlin, GermanySchulz, Hans-Martin;GFZ German Research Centre for Geosciences, Potsdam, Germany Contact Contributors Microprobe Lab (GFZ German Research Centre for Geosciences, Germany); The Potsdam Ion Microprobe (SIMS) User Facility (GFZ German Research Centre for Geosciences, Germany); Elements and Minerals of the Earth Laboratory (ElMiE-Lab) (GFZ German Research Centre for Geosciences, Germany); Microscopy Laboratory (GFZ German Research Centre for Geosciences, Germany)
Funders Petroleum Technology Development Fund:
PhD OSS co-financed with DAAD (57473408)
German Academic Exchange Service:
PhD OSS co-financed with DAAD (57473408)
Helmholtz Association:
Helmholtz-Rekrutierungsinitive to S. Gleeson Society of Economic Geologists Foundation:
Student Research Grant Spora’s Explorers Fund to H. M. Grema (SRG 22-19)
Keywords , compound material > rock > sedimentary rock > clastic sedimentary rock > conglomerate, compound material > rock > sedimentary rock > clastic sedimentary rock > diamictite, compound material > rock > sedimentary rock > clastic sedimentary rock > mudstone, Phanerozoic > Paleozoic More Metadata datacite:
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The main host units comprise the Late Ordovician to Early Silurian Duo Lake Formation and the Middle to Late Devonian Portrait Lake Formation. Sulfide mineralization is hosted in mudstones, conglomerates, diamictites, and volcaniclastic rocks, with stratabound, vein, and breccia-hosted sulfides consisting of sphalerite, pyrite, galena, with minor chalcopyrite and sulfosalts.
This data publication comprises results of analyses conducted on drill core samples obtained from the Boundary Zone. The data originates from multi-scale petrographic examination, quantitative X-ray diffraction (QXRD), electron probe microanalysis (EPMA), and secondary ion mass spectrometry (SIMS) U-Pb fluorapatite geochronology. 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