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ESR 2007-10

Sandstone-Hosted Uranium Potential of Southern Alberta Preliminary Assessment

Sandstone-hosted uranium, the past and present exploration model, is a type of deposit that hosts 30 per cent of world uranium reserves (International Atomic Energy Agency, 2003). The geological setting of southern Alberta has much in common with ... Show Abstract

Matveeva, T.M.  Anderson, S.D.A.  2007-11-01

DIG 2013-0018

Bedrock Geology of Alberta (GIS data, polygon features)

Bedrock Geology of Alberta (GIS data, polygon features) Mapping in support of the dataset included field observations and creating three-dimensional models of subsurface stratigraphy based on the interpretation of geophysical logs from oil and gas ... Show Abstract

Prior, G.J.  Hathway, B.  Glombick, P.M.  Pana, D.I.  Banks, C.J.  Hay, D.C.  Schneider, C.L.  Grobe, M.  Elgr, R.  Weiss, J.A.  2013-09-18

DIG 2014-0011

Bedrock Geology of the Foremost Area (NTS 72E) (GIS data, line features)

Mapping included field observations and creating three-dimensional models of subsurface stratigraphy based on the interpretation of geophysical logs from oil and gas wells. Each three-dimensional formation surface was projected to a model of the ... Show Abstract

Glombick, P.M.  2014-04-02

DIG 2016-0042

Permeability Measurements of Upper Cretaceous and Paleogene Bedrock Cores made from 2004-2015 (tabular data, tab-delimited format, to accompany Open File Report 2016-03)

Permeability Measurements of Upper Cretaceous and Paleogene Bedrock Cores made from 2004-2015 (tabular data, tab-delimited format, to accompany Open File Report 2016-03) The majority of the core samples are from the Horseshoe Canyon, Battle, ... Show Abstract

Smerdon, B.D.  Hughes, A.T.  Jean, G.  2017-02-23

MAP 568

Bedrock Geology of the Foremost Area (NTS 72E)

The Eastend, Whitemud, Battle, Frenchman, and Ravenscrag, and Cypress Hills formations are restricted to the Cypress Hills, a topographically high region located along the eastern margin of the map sheet.The Belly River Group is comprised of the ... Show Abstract

Glombick, P.M.  2014-04-02

OFR 2011-08

Tops of the Horseshoe Canyon, Wapiti and Battle Formations in the West-Central Alberta Plains: Subsurface Stratigraphic Picks and Modelled Surface

Tops of the Horseshoe Canyon, Wapiti and Battle Formations in the West-Central Alberta Plains: Subsurface Stratigraphic Picks and Modelled Surface Representative geophysical logs are included to demonstrate the criteria used to make picks and to ... Show Abstract

Hathway, B.  2011-07-21

OFR 2009-13

Sandstone-Hosted Uranium in Southern Alberta: Petrographic Descriptions of Exposed Upper Cretaceous and Tertiary Rock Formations

Sandstone-Hosted Uranium in Southern Alberta: Petrographic Descriptions of Exposed Upper Cretaceous and Tertiary Rock Formations Exposed Upper Cretaceous and Tertiary rock formations in southern Alberta were sampled for petrographic study. Grain ... Show Abstract

Matveeva, T.M.  Stepic, J.M.  2010-01-15

OFR 2014-10

Three-Dimensional Hydrostratigraphic Modelling of the Sylvan Lake Sub-Basin in the Edmonton-Calgary Corridor, Central Alberta

The Sylvan Lake sub-basin (SLSB) regional scale groundwater study in central Alberta produced a multilayer hydrostratigraphic model representing the vertical and lateral distribution of depositional patterns in the study area. The SLSB was selected ... Show Abstract

Atkinson, L.A.  Glombick, P.M.  2015-02-03

OFR 2009-17

Preliminary Results of Sediment and Bedrock Coring in the Edmonton-Calgary Corridor, Central Alberta

Preliminary Results of Sediment and Bedrock Coring in the Edmonton-Calgary Corridor, Central Alberta After many years of working together on groundwater-related projects, Alberta Geological Survey and Alberta Environment entered into a partnership ... Show Abstract

Riddell, J.T.F.  Andriashek, L.D.  Jean, G.  Slattery, S.R.  2009-12-21

OFR 1980-10

Geology and Coal Resources of the Upper Part of the Horseshoe Canyon Formation

The upper Horseshoe Canyon Formation in the Red Deer area is studied to determine successive depositional environments and to relate these environments to the development of Carbon and Thompson coals. The succeeding coal-bearing sequence ... Show Abstract

Nurkowski, J.R.  1980-01-01