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| 02597nam 2200421zi 4500 |
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001 | 9.917090 |
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003 | CaOODSP |
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005 | 20230831105202 |
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006 | m o d f |
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007 | cr mn||||||||| |
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008 | 221108t20222022oncab ob f000 0 eng d |
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020 | |a9780660461861 |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | 0 |aeng|beng|bfre |
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043 | |an-cn-nu |
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086 | 1 |aM183-7/6-2022E-PDF |
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100 | 1 |aTremblay, T. |q(Tommy)|eauthor. |
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245 | 10|aNew contributions to the ice-flow chronology in the Boothia-Lancaster Ice Stream catchment area / |cT. Tremblay and M. Lamothe. |
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264 | 1|a[Ottawa] : |bGeological Survey Canada, |c2022. |
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264 | 4|c©2022 |
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300 | |a1 online resource (40 pages) : |bcolour illustrations, maps (chiefly colour). |
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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 |aPreprint, |x2816-7872 ; |v6 |
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504 | |aIncludes bibliographical references (pages 33-40). |
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520 | 3 |a"Within the Boothia-Lancaster Ice Stream (BLIS) catchment area, ice flow patterns were reconstructed based on the synthesis of striation directions and cross-cutting relationships, transport patterns of erratic boulders, glacial landforms, cold-based glacial landsystems, and ice-retreat chronology. New ArcticDEM data, high-definition satellite imagery and multibeam echosounder bathymetric datasets provided increased details on ice flow indicators. Convergent high-velocity ice flows through the BLIS main axis were major, persistent features in the northeastern Laurentide Ice Sheet through the last glaciation, and this study highlights intensity fluctuations and ice flow pattern variations that occurred during that time. Highly contrasting glacial geomorphology, notably in the abundance of moraines, reflects marked differences in ice-margin retreat rates and patterns during deglaciation between the western and eastern sides of the BLIS"--Abstract, page 1. |
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546 | |aIncludes abstracts in English and French. |
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650 | 0|aGlacial epoch|zNunavut. |
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650 | 0|aGeological time|zNunavut. |
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650 | 0|aGlacial landforms|zNunavut. |
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650 | 6|aÉpoque glaciaire|zNunavut. |
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650 | 6|aGéochronologie|zNunavut. |
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650 | 6|aGéomorphologie glaciaire|zNunavut. |
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710 | 2 |aGeological Survey of Canada, |eissuing body. |
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830 | #0|aPreprint (Geological Survey of Canada)|v6.|w(CaOODSP)9.913739 |
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856 | 40|qPDF|s46.33 MB|uhttps://publications.gc.ca/collections/collection_2023/rncan-nrcan/M183-7-6-2022-eng.pdf |
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856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/331062 |
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