GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleHelicopter time-domain electromagnetic data over the Eastern Hatfield buried-valley aquifer system, Saskatchewan
DownloadDownloads
AuthorOldenborger, G A; Sharpe, D R; Pugin, A J -M; Russell, H A J
SourceGeological Survey of Canada, Current Research (Online) no. 2013-13, 2013, 18 pages, https://doi.org/10.4095/292517
Year2013
PublisherNatural Resources Canada
Documentserial
Lang.English
Mediaon-line; digital
File formatpdf
ProvinceSaskatchewan
NTS62K/05SE; 62K/05NE; 62K/06SW; 62K/06NW; 62K/11SW; 62K/12SE; 62K/12NW; 62K/13SW; 62L/09NE; 62L/16
AreaMoosomin; Esterhazy; Rocanville
Lat/Long WENS-102.3333 -101.4167 55.2167 50.5833
Subjectshydrogeology; geophysics; groundwater; groundwater resources; aquifers; buried valleys; electromagnetic mapping; e m surveys; conductivity; conductivity surveys; groundwater flow; Eastern Hatfield buried-valley aquifer system
Illustrationslocation maps; profiles; plots; schematic diagrams; seismic sections
ProgramAquifer Assessment & support to mapping, Groundwater Geoscience
Released2013 11 01
AbstractBuried-valley aquifers occur across the Canadian Prairies with a lack of surface expression and complicated network geometries. As part of an effort to map and characterize the Hatfield buried-valley aquifer, the Geological Survey of Canada commissioned a helicopter time-domain electromagnetic survey consisting of 2617 line-km of data over 940 km2 near Esterhazy and Rocanville in southeastern Saskatchewan. Survey results are presented as apparent-conductivity maps and as 3D conductivity-depth models. The Hatfield and Rocanville buried valleys are clearly imaged along with several other erosional and depositional features, some of which have been previously identified at the local scale and are currently utilized as groundwater resources, but for which the extent has not been fully mapped. Other features identified in the survey represent potentially new groundwater resources and can be used to help unravel the details of valley formation, groundwater flow, and aquifer recharge.
GEOSCAN ID292517