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| 001 | 9.919193 |
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| 003 | CaOODSP |
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| 005 | 20230419112929 |
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| 006 | m o d f |
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| 007 | cr cn||||||||| |
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| 008 | 230116t20232023oncdab ob f000 0 eng d |
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| 020 | |a9780660471099 |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn-on |
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| 086 | 1 |aM183-2/8936E-PDF |
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| 100 | 1 |aSlattery, S. R., |eauthor. |
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| 245 | 10|aTunnel-channel complexes in the Zephyr area, Ontario : |bpotential high-yield aquifers / |cS.R. Slattery, P.J. Barnett, A.J.-M. Pugin, D.R. Sharpe, D.R. Goodyear, R.E. Gerber, S. Holysh, and S. Davies. |
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| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2023. |
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| 264 | 4|c©2023 |
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| 300 | |a1 online resource (42 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 ; |v8936 |
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| 504 | |aIncludes bibliographical references (pages 23-26). |
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| 520 | |a"In south-central Ontario, tunnel channels are primary targets for groundwater exploration due to their potential to contain confined, water-bearing, coarse-grained sediment fills. Despite extensive hydrogeologic and geologic exploration within these features, a comprehensive depositional model that illustrates the spatial distribution of coarse- and fine- grained sediment in tunnel-channel complexes is absent. Work in the Zephr area, north of ORM, presents new subsurface data to improve understanding of this geologic setting and to add to geologic models of these channel systems"--Abstract. |
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| 650 | 0|aGroundwater|xResearch|zOntario|zSimcoe, Lake, Region. |
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| 650 | 0|aEau souterraine|xRecherche|zOntario|zSimcoe, Région du lac. |
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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 ; |v8936.|w(CaOODSP)9.506878 |
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| 856 | 40|qPDF|s40.91 MB|uhttps://publications.gc.ca/collections/collection_2023/rncan-nrcan/m183-2/M183-2-8936-eng.pdf |
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| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/331410 |
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