| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.956790 |
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| 003 | CaOODSP |
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| 005 | 20251031143336 |
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| 006 | m o d f |
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| 007 | cr |n||||||||| |
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| 008 | 251028t20132013onc o f|0| 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn-nt|an-cn-nu |
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| 086 | 1 |aM183-2/7352E-PDF |
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| 100 | 1 |aJefferson, Charles Wilson,|d1949- |eauthor. |
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| 245 | 10|aLIPS and Proterozoic uranium (U) deposits of the Canadian Shield / |cC.W. Jefferson, T. Peterson, V. Tschirhart, W. Davis, J.M.J. Scott, K. Reid, P. Ramaekers, S.S. Gandhi, W. Bleeker, S. Pehrsson, W.A. Morris, M. Fayek, E. Potter, N. Bridge, E. Grunsky, P. Keating, K. Ansdell, and N. Banerjee. |
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| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2013. |
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| 264 | 4|c©2013 |
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| 300 | |a1 online resource (4 unnumbered pages). |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aOpen file ; |v7352 |
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| 520 | |a"Most large igneous provinces (LIPs) are associated with lithospheric extension driven by mantle upwelling. The Dubawnt Supergroup LISP (Large Igneous and Sedimentary Province) contains two LIPs and a BLIP of mantle-sourced magmatism likely driven by lithosphere plateau collapse and strike-slip deformation rather than plumes"--Abstract. |
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| 650 | 0|aIgneous rocks|zNorthwest Territories. |
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| 650 | 0|aIgneous rocks|zNunavut. |
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| 650 | 6|aRoches ignées|zTerritoires du Nord-Ouest. |
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| 650 | 6|aRoches ignées|zNunavut. |
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| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
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| 830 | #0|aOpen file (Geological Survey of Canada)|v7352.|w(CaOODSP)9.506878 |
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| 856 | 40|qPDF|s87.60 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7352-eng.pdf |
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| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/292377 |
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