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| 03105cem 2200409za 4500 |
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| 001 | 9.858485 |
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| 003 | CaOODSP |
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| 005 | 20221107160016 |
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| 006 | m go c f |
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| 007 | cr ||||||||||| |
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| 008 | 180704s2014 abc bd a fo 0 eng d |
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| 020 | |a978-1-100-20903-6 |
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| 034 | 1 |aa|b100000|dW127000|eW126000|fN064300|gN064000 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-nt |
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| 086 | 1 |aM183-1/96-2012E-PDF |
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| 100 | 1 |aFallas, K. M., |eauthor. |
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| 245 | 10|aGeology, Carcajou Canyon (southeast), Northwest Territories |h[electronic resource] / |c[Authors: K.M. Fallas and R.B. MacNaughton]. |
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| 255 | |aScale 1:100,000 ; |bUniversal Transverse Mercator, zone 9 |c(W 127°00’--W 126°00'/N 64°30'--N 64°00’) |
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| 260 | |aCalgary Alberta : |bNatural Resources Canada, |c2014. |
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| 300 | |a1 map : |bcol. + |e1 map information document ([18] p.). |
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| 490 | 1 |aCanadian geoscience map ; |v96 |
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| 500 | |aThis record only includes the map and the “Map information document” in PDF, the complete data set with all the files in various formats is available for free download at http://geoscan.nrcan.gc.ca/ |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |a"The southeast quadrant of Carcajou Canyon map area (NTS 96-D) lies within the mountainous Canyon Ranges of the eastern Mackenzie Mountains, Northwest Territories. Outcrop is widespread on the higher ridges in the western portion of the map, but decreases to the northeast as ridges become lower and more vegetated toward the Mackenzie Plain. Rock types include siliciclastic, carbonate, and evaporite strata ranging from Neoproterozoic to Paleocene. Proterozoic and Paleozoic strata have been deformed by northwest- to southeast-trending folds and contractional faults associated with Cordilleran deformation. A set of approximately north-trending minor extensional faults are preserved within Proterozoic and Cambrian strata, and were locally reactivated by Cordilleran deformation. Cryogenian igneous activity resulted in the emplacement of gabbroic dykes into strata of the Mackenzie Mountains Supergroup. Two major unconformities represent significant gaps in the local geological record, one between Proterozoic (Cryogenian) and Cambrian strata, and another between Devonian and Cretaceous strata"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aGeological maps |
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| 692 | 07|2gccst|aGeomorphology |
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| 692 | 07|2gccst|aSurficial geology |
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| 700 | 1 |aMacNaughton, Robert Bruce, |d1968- |econtributor. |
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| 710 | 1 |aCanada. |bNatural Resources Canada, |eissuing body. |
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| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
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| 830 | #0|aCanadian geoscience map ;|v96.|w(CaOODSP)9.506260 |
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| 856 | 40|qPDF|s43.79 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-96-2012-eng.pdf|zMap |
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| 856 | 40|qPDF|s303 KB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-96-2012-1-eng.pdf|zMap information document |
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| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/292288|zGEOSCAN DOI |
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