Resolving Paragneiss Provenance at Grollier Lake in the Athabasca Granulite Terrane, Western Canadian Shield
U-Pb crystallization ages of metamorphic and detrital zircons from all three paragneiss samples fall into the range of ca. 1.85-2.59 Ga, excluding two much older grains. Evidence suggests that the paragneiss of Grollier Lake record deformation exclusively from the Taltson and Trans-Hudson orogenies....
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ScholarWorks@UARK
2016
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Online Access: | https://scholarworks.uark.edu/etd/1563 https://scholarworks.uark.edu/context/etd/article/3102/viewcontent/Ply_uark_0011O_12122.pdf |