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| 02196cem 2200397za 4500 |
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| 001 | 9.576719 |
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| 003 | CaOODSP |
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| 005 | 20221107134047 |
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| 006 | m go c f |
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| 007 | cr ||||||||||| |
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| 008 | 150406s2013 onc bd a fo 0 eng d |
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| 020 | |a978-1-100-22352-0 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-nu|an-cn-nt |
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| 086 | 1 |aM183-1/75-2013E-PDF |
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| 245 | 00|aTectonic assemblage map of Hadley Bay |h[electronic resource] : |bVictoria and Prince of Whales islands, Nunavut-Northwest Territories / |c[by] R.H. Rainbird ... [et al.]. |
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| 250 | |aPreliminary version |
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| 255 | |aScale 1:50,000 |
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| 260 | |aOttawa : |bNatural Resources Canada, |cc2013. |
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| 300 | |a1 map : |bcol. |
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| 490 | 1 |aCanadian geoscience map ; |v75 |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |a"This map and the related geodatabase illustrate the bedrock geology of central and northeastern Victoria Island, Stefansson Island, and western Prince of Wales Island. Major features of the area include inliers of Neoarchean basement granitoid rocks; clastic rock-dominated sections associated with the late Paleoproterozoic Kilohigok Basin, and Mesoproterozoic Elu Basin; extensive Meso- and Neoproterozoic strata of Amundsen Basin, diabase sills, and extrusive basaltic rocks related to the Franklin Large Igneous Province (ca. 723 Ma) and unconformable Cambrian to Devonian strata of Arctic Platform"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 590 | |a14-16|b2014-04-17 |
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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 |aRainbird, Robert H. |q(Robert Howard), |d1957- |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 794 | |tGeology, tectonic assemblage map of Hadley Bay, Victoria and Prince of Wales Islands, Nunavut–Northwest Territories |w(CaOODSP)9.557276 |
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| 830 | #0|aCanadian geoscience map ;|v75.|w(CaOODSP)9.506260 |
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| 856 | 40|qPDF|s7.65 MB|uhttps://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-75-2013-eng.pdf |
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| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/292820 |
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