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SPE 090

Subsurface Characterization of Acid-Gas Injection Operations in the Peace River Arch Area, 2007

In the cases of acid-gas injection into deep saline aquifers (Gordondale-Belloy, Mulligan, Pouce Coupe, Rycroft and Wembley), the extent and migration of the acid-gas plume will likely be limited by dissolution, dispersion, residual gas saturation ... Show Abstract

Michael, K.  Buschkuehle, B.E.  2008-03-01

ECO 4

Limestone resources of Alberta

Seven areas in Alberta, close to transportation facilities, were studied to determine quality and reserves of high-calcium limestone.Three formational units in the foothills and mountain regions are of importance. Formerly a cement plant operated ... Show Abstract

Holter, M.E.  1976-01-01

ESN 1977-A

Stoneware and low duty refractory clays associated with the Athabasca Oil Sands

Open-pit mining of the Athabasca Oil Sands in the Fort McMurray area removes most of the overburden from basal McMurray Formation clays which have potential for use as stoneware and low heat duty refractories. The clays have good plasticity and ... Show Abstract

Scafe, D.W.  1977-01-01

ECO 2

Alberta Bentonites

Low yields, high grit content, or thick overburden reduce the desirability of other deposits.The paucity of glass shards and the mineralogy of the sand and silt fractions suggest rhyodacite as the composition of the parent volcanic ash for each ... Show Abstract

Scafe, D.W.  1975-01-01

SPE 097

Geochemical, Mineralogical and Kimberlite Indicator Mineral Electron Microprobe Data from Silts, Heavy Mineral Concentrates and Waters from National Geochemical Reconnaissance Stream Sediment and Water Surveys in the Northeastern and Southern Clear Hills

The Alberta Geological Survey and the Geological Survey of Canada have conducted cooperative reconnaissance-scale sampling of tills, stream sediments and waters in northern Alberta to assess potential for kimberlite (diamonds), base metals and other ... Show Abstract

McCurdy, M.W.  Prior, G.J.  Day, S.J.A.  Weiss, J.A.  Friske, P.W.B.  Pawlowicz, J.G.  McNeil, R.J.  Hathway, B.  Wilson, R.S.  Goulet, D.E.  2008-06-05

SPE 088

Deep electrical structure of Buffalo Head Hills, Northern Alberta: Implications for diamond exploration

Geophysical studies in the Northwest Territories have shown that diamondiferous kimberlite pipes are spatially coincident with a zone of high electrical conductivity in the upper mantle. The apparent spatial coincidence between diamondiferous ... Show Abstract

Turkoglu, ErsanUnsworth, MartynPana, D.I.  2007-05-01

SPE 108

Petrographic Analysis of Selected Alberta Strata (Cardium, Viking, Banff, Exshaw, Duvernay, Slave Point)

Petrographic Analysis of Selected Alberta Strata (Cardium, Viking, Banff, Exshaw, Duvernay, Slave Point) Sixty-five thin sections were sent to Trican Geological Solutions Ltd. for description and photographs according to specific criteria outlined ... Show Abstract

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

ECO 5

Bromide, iodide and boron in Alberta formation waters

Bromide contents up to 2786 mg/L were found in high calcium and magnesium brines associated with evaporites in the Upper Devonian Beaverhill Lake Formation and Middle Devonian Elk Point Group. The most extensive regions of high-iodide formation ... Show Abstract

Hitchon, B.  Levinson, A.A.  Horn, M.K.  1977-01-01

MAP 602

Bedrock Topography of Alberta, Canada

Bedrock Topography of Alberta, Canada Explanatory notes, references, and data sources appear on a supplementary page to accompany the map. Place Keywords 72e 72l 72m 73d 73e 73l 73m 74d 74e 74l 74m 82g 82h 82i 82j 82n 82o 82p 83a 83b 83c 83d 83e ... Show Abstract

MacCormack, K.E.  Atkinson, N.  Lyster, S.  2015-05-12

ECO 7

The ceramic potential of Alberta clays and shales

Many geographical areas and geological formations were missed when the ceramic suitability of materials was studied early this century. Geological formations that are useful for the production of structural clay products or pottery are Pleistocene ... Show Abstract

Scafe, D.W.  1982-01-01

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