| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.956460 |
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| 003 | CaOODSP |
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| 005 | 20251031142449 |
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| 006 | m o d f |
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| 007 | cr |n||||||||| |
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| 008 | 251017t20152015oncdab ob f|0| 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn-nu |
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| 086 | 1 |aM183-2/7874E-PDF |
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| 100 | 1 |aLeBlanc, A.-M., |eauthor. |
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| 245 | 10|aDInSAR interannual seasonal surface displacement in permafrost terrain, Iqaluit, Nunavut / |cA.-M. LeBlanc, N. Short, V. Mathon-Dufour, and J. Chartrand. |
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| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2015. |
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| 264 | 4|c©2015 |
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| 300 | |a1 online resource (33 pages) : |bcharts, illustrations, maps. |
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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, |x2816-7155 ; |v7874 |
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| 504 | |aIncludes bibliographical references (pages 17-18). |
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| 520 | |a"In recent years, interest in the use of Interferometric Synthetic Aperture Radar (InSAR) as a surface displacement assessment tool for permafrost environments has increased considerably. Among the available InSAR methods, conventional differential InSAR (DInSAR) makes it possible to detect very small ground surface movement, on the order of centimetres, for every pixel over large areas, providing a way to assess active layer and permafrost dynamics"--Introduction, page 4. |
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| 650 | 0|aPermafrost|zNunavut. |
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| 650 | 0|aInterferometry. |
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| 650 | 6|aPergélisols|zNunavut. |
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| 650 | 6|aInterférométrie. |
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| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
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| 830 | #0|aOpen file (Geological Survey of Canada)|x2816-7155 ;|v7874.|w(CaOODSP)9.506878 |
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| 856 | 40|qPDF|s4.34 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7874-eng.pdf |
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| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/297406 |
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