Abstract: Neoproterozoic to Cambrian siliciclastic rocks in the Barn Mountains, Yukon are stratigraphically similar to coeval strata on the northwest Laurentian margin and the North Slope subterrane of the Arctic Alaska terrane. Sandstone samples collected for detrital zircon U/Pb geochronology from Oldhamia-bearing sections in the Barn Mountains yield age spectra with major Paleoproterozoic and subordinate Mesoproterozoic and Archean peaks that are compatible with a Laurentian cratonal provenance. Comparison of data from the Barn Mountains with available data from the Laurentian margin is permissive of derivation from either the northwestern or the north to northeastern margin of Laurentia.

Authors: McClelland, W.C., Colpron, M., Peipjohn, K., von Gosen, W., Ward, W. and Strauss, J.V.

Citation: McClelland, W.C., Colpron, M., Peipjohn, K., von Gosen, W., Ward, W. and Strauss, J.V., 2015. Preliminary detrital zircon geochronology of the Neruokpuk Formation in the Barn Mountains, Yukon. In: Yukon Exploration and Geology 2014, K.E. MacFarlane, M.G. Nordling and P.J. Sack (eds.), Yukon Geological Survey, p. 123-143.

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