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008	241003t20242024oncbdo  ob   f000 0 eng d
020	|a9780660738963
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-on|an-cn-qu
086	1 |aM183-2/9219E-PDF
100	1 |aPugin, A. J-M., |eauthor.
245	10|aOrigin of mass movements and faulted glaciolacustrine deposits in the upper Lake Timiskaming area, Ontario-Quebec, using high-resolution seismic reflection / |cA.J.-M. Pugin, G.R. Brooks, and K. Brewer.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2024.
264	4|c©2024
300	|a1 online resource (32 pages) : |bmaps, graphs, photographs.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v9219
504	|aIncludes bibliographical references (pages 30-32).
520	3 |a"Three high-resolution seismic surveys were conducted over upper Lake Timiskaming in 2019, 2021 and 2022 using a new penetrative technology developed at the Geological Survey of Canada. The goal of these surveys was to investigate the origin of previously reported faulted glaciolacustrine sediments. Such deformation structures may be related to the collapse of slow melting buried ice, gravity mass movements, or deep-seated, bedrock fault movement"--Abstract, page 1.
650	0|aFaults (Geology)|zTimiskaming, Lake (Ont. and Québec)
650	0|aSeismic tomography|zTimiskaming, Lake (Ont. and Québec)
650	6|aFailles (Géologie)|zTémiscamingue, Lac (Ont. et Québec)
650	6|aTomographie sismique|zTémiscamingue, Lac (Ont. et Québec)
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v9219.|w(CaOODSP)9.506878
856	40|qPDF|s44.9 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-9219-eng.pdf
856	40|qHTML|sN/A|uhttps://doi.org/10.4095/p0f205dx57