| 000 | 00000cam 2200000zi 4500 |
| 001 | 9.953883 |
| 003 | CaOODSP |
| 005 | 20260916102253 |
| 006 | m o d f |
| 007 | cr cn||||||||| |
| 008 | 250807t20262026oncab ob f000 0 eng d |
| 020 | |a9780660783970 |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-nu |
| 086 | 1 |aM183-2/9289E-PDF |
| 100 | 1 |aOldenborger, G. A. |q(Greg A.)|eauthor. |
| 245 | 10|aElectromagnetic mapping of sublacustrine saline permafrost, Rankin Inlet, Nunavut / |cG.A. Oldenborger. |
| 264 | 1|a[Ottawa] : |bNatural Resources Canada = Ressources naturelles Canada, |c2026. |
| 264 | 4|c©2026 |
| 300 | |a1 online resource (ii, 22 pages) : |bcolour illustrations, colour maps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aGeological Survey of Canada open file, |x2816-7155 ; |v9289e |
| 500 | |aIssued also in French under title: Cartographie électromagnétique du pergélisol salin sous‑lacustre, Rankin Inlet (Nunavut). |
| 504 | |aIncludes bibliographical references (pages 7-8). |
| 520 | |a"An electromagnetic geophysical survey was conducted over First Landing Lake in the vicinity of Rankin Inlet, Nunavut as part of a study on lake taliks. Survey results show areas of high electrical conductivity associated with the shallow lake terrace. High electrical conductivity is interpreted to result from sublacustrine saline permafrost. Saline permafrost will have a direct influence on permafrost dynamics and lake talik formation"--Summary, page i. |
| 650 | 0|aPermafrost|zNunavut. |
| 650 | 0|aElectromagnetic fields|zNunavut|xMeasurement. |
| 650 | 0|aGeophysical surveys|zNunavut. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 775 | 08|tCartographie électromagnétique du pergélisol salin sous‑lacustre, Rankin Inlet (Nunavut) / |w(CaOODSP)9.959175 |
| 830 | #0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v9289e.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s4.26 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-9289-eng.pdf |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/pqunx9q1bk |