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008	250207t20252025oncb    ob   f000 0 eng d
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040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-nt
086	1 |aM183-2/9149E-PDF
100	1 |aHadlari, T., |d1974- |eauthor.
245	10|aU-Pb detrital zircon data from lower Cretaceous strata near the Mackenzie Mountain front, Northwest Territories / |cT. Hadlari and L.M. Heaman.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2025.
264	4|c©2025
300	|a1 online resource (5 pages) : |bmaps.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v9149
504	|aIncludes bibliographical references (page 5).
520	|a"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.
650	0|aZircon|zNorthwest Territories|xAnalysis.
650	0|aFormations (Geology)|zNorthwest Territories.
650	6|aZircon|zTerritoires du Nord-Ouest|xAnalyse.
650	6|aFormations (Géologie)|zTerritoires du Nord-Ouest.
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v9149.|w(CaOODSP)9.506878
856	40|qPDF|s758 KB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-9149-eng.pdf
856	4 |qHTML|sN/A|uhttps://doi.org/10.4095/pssp20ap8e