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TitleL'utilisation du géoradar et des méthodes électriques pour la cartographie des formations aquifères du piémont laurentien, Québec
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AuthorMichaud, Y; Fortier, R; Parent, M; Pilon, J
SourceCurrent Research 1997-E/Recherches en cours 1997-E; by Geological Survey of Canada; Geological Survey of Canada, Current Research 1997-E, 1997 p. 73-82, https://doi.org/10.4095/209081 (Open Access)
Year1997
PublisherNatural Resources Canada
Documentserial
Lang.French
Mediapaper; on-line; digital
RelatedThis publication is contained in Geological Survey of Canada; (1997). Current Research 1997-E, Geological Survey of Canada, Current Research no. 1997-E
File formatpdf
ProvinceQuebec
NTS21L/13
AreaPont-Rouge; Saint-Léonard-de-Portneuf; Rivière Saint-Anne; Rivière Jacques-Cartier; Saint-Raymond; Laurentian piedmont
Lat/Long WENS -71.9953 -71.5719 46.9439 46.7428
Subjectsgeophysics; stratigraphy; hydrogeology; aquifers; ground probing radar; geophysical surveys; radar methods; electrical surveys; resistivity; i p interpretations; i p surveys; stratigraphic analyses; moraines; glacial deposits; geophysical interpretations; water table; Saint-Narcisse Moraine; Quaternary
Illustrationssketch maps; radar profiles; analyses
Released1997 07 01
AbstractGeophysical investigations are being conducted to complement stratigraphic data on Quaternary sequences of the Laurentian piedmont and to evaluate the potential and limitations of selected geophysical methods for the delineation of aquifers in surficial deposits. Ground penetrating radar (GPR), electrical resistivity, and induced polarization have been used on surface aquifers in Sainte-Anne River delta in the Jacques-Cartier River delta, and in the vicinity of the Saint-Narcisse Moraine. Results show that these geophysical methods are complementary and that they can be used to identify different stratigraphic units and to determine their lateral extent and their organization. They can also be used to determine the depth of the water table.
GEOSCAN ID209081