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DIG 2016-0044

Relative Landslide Susceptibility Model of the Alberta Plains and Shield Regions (gridded data, geotiff format)

Importantly, it does not evaluate the probability of landslide occurrence over any specific period of time, nor does it evaluate the magnitude or impact of any potential landslide activity. [...]the model results should not be interpreted for the ... Show Abstract

Pawley, S.  Hartman, G.M.D.  Chao, D.K.  2016-12-15

DIG 2016-0040

Compilation of In Situ Stress Data from Alberta and Northeastern British Columbia (tabular data, tab delimited)

Understanding the state of stress in the subsurface has always been important in the development of energy resources. The recent development of unconventional oil sand and low permeability hydrocarbon deposits, waste fluid disposal, greenhouse gas ... Show Abstract

Haug, K.  Bell, J.S.  2016-08-09

OFR 2018-06

Geochronology in Support of the Alberta Table of Formations: Rhenium-Osmium Isotope Dating of Selected Devonian and Jurassic Core Samples from Central and Northern Alberta

Geochronology in Support of the Alberta Table of Formations: Rhenium-Osmium Isotope Dating of Selected Devonian and Jurassic Core Samples from Central and Northern Alberta The samples were collected from core hosted by the Alberta Energy Regulator ... Show Abstract

Pana, D.I.  Creaser, R.A.  Toma, J.  Playter, T.L.  Corlett, H.  Hauck, T.E.  Peterson, J.T.  Grobe, M.  Poulton, T.P.  2018-06-05

SPE 102

Limestone and Dolomite Prospects for Industrial Use in the Alberta Foothills and Front Ranges

Limestone and Dolomite Prospects for Industrial Use in the Alberta Foothills and Front Ranges The specific purpose of this report was to provide geoscience information on limestone and dolomite prospects to help guide land use planning ... Show Abstract

Krueger, K.  Kluczny, P.  Dahrouge, J.R.  2016-07-20

SPE 103

Diamond Potential in Alberta: Distribution of Kimberlite and Kimberlite Indicator Mineral Clusters

Diamond Potential in Alberta: Distribution of Kimberlite and Kimberlite Indicator Mineral Clusters The specific purpose of this report was to provide geoscience information on Alberta's diamond potential to help guide land-use planning. Two known ... Show Abstract

Banas, A.  Eccles, D.R.  Dufresne, M.B.  2016-07-20

BUL 066

Geostatistical Rendering of the Architecture of Hydrostratigraphic Units within the Paskapoo Formation, Central Alberta

Geostatistical Rendering of the Architecture of Hydrostratigraphic Units within the Paskapoo Formation, Central Alberta The Paskapoo Formation is one of the largest and most intensely used bedrock aquifer systems in Alberta, yet little is known ... Show Abstract

Lyster, S.  Andriashek, L.D.  2012-08-03

OFR 2017-07

First-Order Groundwater Availability Assessment for Central Alberta

First-Order Groundwater Availability Assessment for Central Alberta The aquifer-yield continuum classifies groundwater yield along a spectrum that helps define total groundwater availability and is bound by two extremes: non-use and maximum ... Show Abstract

Klassen, J.  Smerdon, B.D.  2018-02-14

SPE 107

Hydrocarbon Analysis by Thermal Desorption Gas Chromatography on Selected Alberta Strata (Viking, Westgate, Cardium, Wilrich, Exshaw)

Hydrocarbon Analysis by Thermal Desorption Gas Chromatography on Selected Alberta Strata (Viking, Westgate, Cardium, Wilrich, Exshaw) Six core samples, from five well locations in Alberta, were sent to Trican Geological Solutions Ltd. for thermal ... Show Abstract

Pawlowicz, J.G.  Anderson, S.D.A.  Rokosh, C.D.  2017-09-28

DIG 2017-0024

Groundwater Yield Matrix for Central Alberta (GIS data, polygon features)

Groundwater Yield Matrix for Central Alberta (GIS data, polygon features) The classes within the yield matrix from most conservative to maximum mining are: permissive sustained yield, maximum sustained yield, sustained yield, permissive mining ... Show Abstract

Klassen, J.  Smerdon, B.D.  2018-02-14

ESR 2002-04

Hydrogeology and Stress Regime of the Upper Cretaceous-Tertiary Coal-Bearing Strata in Alberta

The flow of formation waters in these strata is driven by gravity (topography) and erosional rebound, and is controlled by rock absolute permeability, gas generation and capillary pressure to gas (relative permeability). The gas content of the coal ... Show Abstract

Bachu, S.  Michael, K.  2002-10-01

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