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020 |a9780660401195
040 |aCaOODSP|beng|erda|cCaOODSP
0410 |aeng|beng|bfre
043 |an-cn-nt
0861 |aM44-2022/2E-PDF
1001 |aFallas, K. M., |eauthor.
24510|aAge dating of a bentonite in the Duo Lake Formation, western Mackenzie Mountains, Northwest Territories / |cK.M. Fallas and W. Matthews.
264 1|a[Ottawa] : |bGeological Survey of Canada, |c2022.
264 4|c©2022
300 |a1 online resource (14 pages) : |billustrations (some colour), colour map.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aCurrent research, |x1701-4387 ; |v2022-2
504 |aIncludes bibliographical references (pages 12-14).
5203 |a"In the Misty Creek Embayment of the western Mackenzie Mountains, Duo Lake Formation locally includes minor volcanic deposits associated with Marmot Formation volcanism. A bentonite layer from an outcrop of graptolitic shale found in NTS map area 106-B, in the upper part of the Duo Lake Formation, was sampled for U-Pb zircon dating. Analytical results yielded a dominant population of grains with a concordia age of 439.8 ± 3.0 Ma, interpreted as the age of deposition. Minor inherited zircon populations yielded ages ranging from approximately 1200 to 2850 Ma. Observed graptolites from the same outcrop likely range from Middle Ordovician to Early Silurian and are compatible with the interpreted U-Pb age of the bentonite. Previously known Middle and Late Ordovician volcanic activity in the Misty Creek Embayment is here expanded to include Early Silurian activity, and serves as a proxy for the timing of active extensional tectonism in the basin"--Abstract, page 1.
546 |aIncludes abstracts in English and French.
650 0|aBentonite|zNorthwest Territories.
650 0|aUranium-lead dating|zNorthwest Territories.
650 3|aBentonite|zTerritoires du Nord-Ouest.
650 3|aDatation|xMéthode uranium-plomb|zTerritoires du Nord-Ouest.
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aCurrent research (Geological Survey of Canada)|v2022-2.|w(CaOODSP)9.506236
85640|qPDF|s22.18 MB|uhttps://publications.gc.ca/collections/collection_2022/rncan-nrcan/M44-2022-2-eng.pdf
8564 |qHTML|sN/A|uhttps://doi.org/10.4095/328830