U-Pb detrital zircon data from lower Cretaceous strata near the Mackenzie Mountain front, Northwest Territories / T. Hadlari and L.M. Heaman. : M183-2/9149E-PDF

"Three sandstone samples were collected from lower Cretaceous strata in the northern Mackenzie Valley region. The sampled stratigraphy includes: the Tukweye Member of the Martin House Formation, which is an incised valley deposit at the base of the Cretaceous succession; marine facies of the Martin House Formation, a widespread transgressive sandstone above the sub-Cretaceous unconformity; and the Sans Sault Member of the Arctic Red Formation, which is a marine sandstone at the top of the lower Cretaceous (Albian) succession. These samples were analysed at the University of Alberta for U-Pb detrital zircon isotopic age dating. The analytical results are presented here and the full provenance interpretation will be presented in a subsequent publication"--Abstract, page 2.

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