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| 01864cam 2200325za 4500 |
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| 001 | 9.804456 |
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| 003 | CaOODSP |
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| 005 | 20221107135424 |
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| 007 | cr ||||||||||| |
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| 008 | 150406s1991 onc|||||o f|0| 0 eng d |
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| 020 | |q(paper)|z0-660-13838-7 |
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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 |aM42-404E-PDF |
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| 100 | 1 |aAitken, J.D. |
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| 245 | 14|aThe Ice Brook Formation and post-Rapitan, late Proterozoic glaciation, Mackenzie Mountains, Northwest Territories |h[electronic resource] / |cJ.D. Aitken. |
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| 260 | |aOttawa : |bEnergy, Mines and Resources Canada : |bGeological Survey of Canada, |cc1991. |
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| 300 | |a[5], 43 p. : |bmaps, figs. |
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| 490 | 1 |aBulletin / Geological Survey of Canada |v404 |
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| 500 | |aThe catalogue number (M42-404E) and ISBN (0-660-13838-7) for the print edition have been copied in this electronic publication. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 0 |a"In the Mackenzie Mountains, glacial influence on deposition of the Upper Proterozoic Sayunei formations of the Rapitan Group has been well documented. Until recently, these havebeen considered the only Proterozoic glacial deposits of the region. This report documents the evidence for glacial origin of Upper Proterozoic diamictites occurring one kilometre or more stratigraphically above the Rapitan. These younger diamictites previously were thought to be the result of mass flow processes."--Summary, p. 3. |
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| 692 | 07|2gccst|aGlaciers |
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| 692 | 07|2gccst|aSedimentary rock |
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| 692 | 07|2gccst|aGeology |
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| 710 | 1 |aCanada. |bEnergy, Mines and Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 830 | #0|aBulletin (Geological Survey of Canada : Online)|v404|w(CaOODSP)9.504778 |
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| 856 | 40|qPDF|s27.45 MB|uhttps://publications.gc.ca/collections/collection_2015/rncan-nrcan/M42-404-eng.pdf |
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