Results : 1 - 10 of 16
DIG 2016-0044
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
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 2015-07
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
SPE 103
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
OFR 2017-07
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
DIG 2017-0024
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
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
MAP 032
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
OFR 2017-02
New data have shed light on some of the earlier uncertainties resulting in improved assumptions and more precise hydrocarbon resources models. The estimates for the total in-place resources in the Duvernay Formation are 22.1 1012m3 to 24.2 1012m3 ... Show Abstract
Lyster, S. Corlett, H. Berhane, H. 2017-07-20
DIG 2016-0009
Mercury Porosimetry Data of Alberta Geological Units for Shale- and Siltstone-Hosted Hydrocarbon Evaluation (tabular data, tab-delimited format) The strata evaluated include the following units: basal Banff Formation, Colorado Group, Montney ... Show Abstract
Rokosh, C.D. Crocq, C.S. Pawlowicz, J.G. Brazzoni, T. 2016-06-10
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