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TitleStudy of groundwater flow patterns in Carboniferous sediments of Atlantic Canada, 021G/1
DownloadDownloads
AuthorWater Management Services Limited; 3-D Geoconsultants Limited; J.A Leslie and Associates Limited
SourceEarth Physics Branch, Open File 84-11, 1984, 45 pages (3 sheets), https://doi.org/10.4095/293621 (Open Access)
Year1984
PublisherEnergy, Mines and Resources Canada (Ottawa, Canada)
Documentopen file
Lang.English
MapsPublication contains 1 map
Map Info.geological, bedrock geology, 1:250,000
Mediapaper; on-line; digital
File formatpdf
ProvinceNew Brunswick
NTS21G/01; 21G/02; 21G/03; 21G/06; 21G/07; 21G/08; 21G/09; 21G/10; 21G/11; 21G/14; 21G/15; 21G/16; 21H/05; 21H/12; 21H/13; 21I/04; 21J/01; 21J/02; 21J/03
AreaFredericton; Saint John; Oromocto; Gagetown; Saint John River; Oromocto River; McAdam; Silverwood; Sussex
Lat/Long WENS -67.5000 -65.5000 46.2500 45.2500
Subjectshydrogeology; geophysics; groundwater; geothermal potential; geothermal temperatures; geothermal gradient; temperature; boreholes; bedrock geology; groundwater flow; heat flow; aquifers; water geochemistry; recharge rates; Fredericton subbasin; Carboniferous
Released1984 01 01; 2019 11 29
AbstractThe Fredericton sedimentary sub-basin forms the westernmost section of the St. Lawrence Plains. The sediments of the sub-basin range in age from Pennsylvanian to Kississippian. The principal structural feature is the Fredericton Graben, a down-faulted black that occupies the northwest quadrant of the basin. The sub-basin displays no large identifiable aquifers. On a large scale, however, the series of sediments that are of limited areal extent display hydraulic continuity. Within the sub-basin groundwater flow occurs in two major directions, northeastwards and eastwards. Known water yields in the upper 200 m vary from 0.076 L/s to 38.0 L/s. Potential aquifers lie at depth, likely in Lower Pennsylvanian and Upper Kississippian sediments. Flows are expected to be in the range 38 to 76 L/s.
GEOSCAN ID293621