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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

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

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

MAP 032

Uppermost Cretaceous and Tertiary Strata of Central and Southern Alberta

The mapped formations are, from youngest to oldest: St. Mary River, Edmonton, Eastend, Willow Creek, Paskapoo, Ravenscrag, Porcupine Hills, Cypress Hills and Handhills. Place Keywords alberta canada 72e 72l 72m 73d 73e 72l 73m 82g 82h 82i 82j 82n ... Show Abstract

Carrigy, M.A.  1971-01-01

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

SPE 099

QEMSCAN Analysis of Various Lithologies from Tight- and Shale-Gas Plays in Alberta

The samples were submitted to SGS's Advanced Reservoir Quality Services (ARQS) team for mineralogical and textural characterization using Quantitative Evaluation of Materials by Scanning Electron Microscopy (QEMSCAN). In order to characterize the ... Show Abstract

Rokosh, C.D.  Anderson, S.D.A.  Pawlowicz, J.G.  2016-09-20

OFR 2015-07

Investigation of Odours and Emissions from Heavy Oil and Bitumen in the Peace River Oil Sands Area: 3-D Geological Modelling and Petroleum Geochemistry

Report of Recommendations on Odours and Emissions in the Peace River Area), and included the creation of a three-dimensional (3-D) geological model, designing and implementing a petroleum sampling and analysis program, and defining geological plays ... Show Abstract

Anderson, S.D.A.  Filewich, C.  Lyster, S.  MacCormack, K.E.  2015-08-04

OFR 2017-02

Hydrocarbon Resource Potential of the Duvernay Formation in Alberta - Update

The 2012 assessment of the Duvernay Formation included only the very earliest test wells in the Duvernay and therefore made many assumptions about rock properties, water saturation, fluid distributions, and pressure and temperature regimes. New ... Show Abstract

Lyster, S.  Corlett, H.  Berhane, H.  2017-07-20

SPE 109

Petrographic Analysis of Selected Alberta Strata (Doe Creek, Dunvegan)

Twenty thin sections produced from core samples from thirteen Alberta wells were sent to Calgary Rock and Materials Services Inc. for description and photographs according to specific criteria requested by the Alberta Geological Survey. The ... Show Abstract

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

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

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