000 02441cem  2200397za 4500
0019.574442
003CaOODSP
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008150406s2013    onc    bd a  fo 0   eng d
020 |a978-1-100-20896-1
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nt
0861 |aM183-1/89-2012E-PDF
1001 |aFallas, K. M., |eauthor.
24510|aGeology, Mahony Lake (northeast), Northwest Territories |h[electronic resource] / |c[by] K.M. Fallas and B.C. MacLean.
255 |aScale 1:100,000
260 |aOttawa : |bNatural Resources Canada, |cc2013.
300 |a1 map : |bcol.
4901 |aCanadian geoscience map ; |vNo. 89
500 |aIncludes a legend.
504 |aIncludes bibliographical references.
5203 |a"This map area, encompassing the northeast quadrant of the Mahony Lake map area (NTS 96-F), lies at the western edge of the Great Bear Plain, between the Franklin Mountains and Great Bear Lake, Northwest Territories. The area is dominated by a low, undulating, forested plain with rare bedrock exposure. Most of the area is underlain by flat-lying Cretaceous sedimentary strata, disturbed locally by minor fold or fault features. Near the western edge of the map area, the Neyele Lake Fault juxtaposes Paleozoic carbonate strata against Cretaceous siliciclastic strata, with little or no topographic relief. Evidence of this fault is found on public-domain seismic-reflection profiles archived with the National Energy Board. The Neyele Lake Fault demarcates the eastern most structural feature at this latitude involving Paleozoic strata that developed as a result of Cordilleran deformation. Historical exploration by petroleum companies in the area targeted potential reservoirs in buried Cambrian strata"--Abstract.
546 |aIncludes abstract in French.
590 |a13-21|b2013-05-24
69207|2gccst|aGeological maps
69207|2gccst|aLakes
69207|2gccst|aSurficial geology
7001 |aMacLean, B. C., |econtributor.
7101 |aCanada. |bNatural Resources Canada, |eissuing body.
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aCanadian geoscience map ;|vNo. 89.|w(CaOODSP)9.506260
85640|qPDF|s7.53 MB|uhttps://publications.gc.ca/collections/collection_2013/rncan-nrcan/M183-1-89-2012-eng.pdf
85640|qHTML|sN/A|uhttps://doi.org/10.4095/292174