00000nem 2200000za 4500 9.574448 CaOODSP 20230131161133 m go c f cr ||||||||||| 150406s2013 onc bd a fo 0 eng|d 978-1-100-20902-9 CaOODSP eng eng fre n-cn-nt M183-1/95-2012E-PDF Fallas, K. M., author. Geology, Carcajou Canyon (northeast), Northwest Territories [electronic resource] / [by] K.M. Fallas, T. Hadlari, and B.C. MacLean. Scale 1:50,000 Ottawa : Natural Resources Canada, c2013. 1 map : col. Canadian geoscience map ; No. 95 Includes bibliographical references. "The northeast quadrant of the Carcajou Canyon map area (NTS 96-D) straddles the Mackenzie Mountains and Mackenzie Plain, Northwest Territories, rising from a relatively flat, low-lying plain in the northeast to mountainous terrain in the southwest. Much of the Mackenzie Plain is here underlain by flat or very gently folded Cretaceous to Paleocene siliciclastic strata. Exposures in the Mackenzie Mountains include siliciclastic and carbonate strata ranging in age from Neoproterozoic to Devonian. These older strata have been brought to surface along compressional faults and in the cores of anticlines associated with Cordilleran deformation. Structural features are dominated by a northwest trend, the exception being the northeast-trending Gambill Fault. Public-domain seismic-reflection lines, archived with the National Energy Board, help constrain the location of contacts between sparsely exposed Cretaceous units. Petroleum exploration by private industry in the area targets Cambrian or Devonian strata in the subsurface of the Mackenzie Plain"--Abstract. Includes abstract in French. 14-16 2014-04-17 gccst Geological maps gccst Geomorphology gccst Surficial geology MacLean, B. C., author. Hadlari, T., 1974- author. Canada. Natural Resources Canada, issuing body. Geological Survey of Canada, issuing body. Canadian geoscience map ; No. 95. (CaOODSP)9.506260 PDF 14.03 MB https://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-95-2012-eng.pdf HTML N/A https://doi.org/10.4095/292287 292287