Dehler, Carol M.Fanning, ChristopherLink, Paul K.Kingsbury, Esther M.Rybczynski, Dan2015-12-100016-7606http://hdl.handle.net/1885/50819U-Pb detrital zircon analyses provide a new maximum depositional age constraint on the Uinta Mountain Group (UMG) and correlative Big Cottonwood Formation (BCF) of Utah, and significantly enhance our insights on the mid-Neoproterozoic paleogeographic andKeywords: Age constraints; Age distribution; Alternative source; Antarctica; Archean; Arizona; Australia; Data support; Detrital zircon; Detrital zircon grains; Grand Canyons; Marine currents; Neoproterozoic; North American; Pacific ocean; Paleogeography; PaleoprotMaximum depositional age and provenance of the Uinta Mountain Group and Big Cottonwood Formation, northern Utah: Paleogeography of rifting western Laurentia201010.1130/B30094.12016-02-24