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ESR 2000-11

Suitability of the Alberta Subsurface for Carbon Dioxide Sequestration in Geological Media

Sequestration of anthropogenic CO2 in geological media is a potential solution to the release into the atmosphere of CO2, a greenhouse gas. Basically, there are five ways of sequestering CO2 in geological media: 1) through enhanced oil recovery ... Show Abstract

Bachu, S.  Brulotte, M.  Grobe, M.  Stewart, S.A.  2000-03-01

ESR 1982-03

Springs of Alberta

The first part of this report looks at the spatial distribution of the springs by region, flow rate, water temperature and water chemistry. In the second part, the report describes in detail several springs that were chosen because of the magnitude ... Show Abstract

Borneuf, D.M.  1983-01-01

ESR 2003-01

Stratigraphy and sedimentology of the Athabasca Group in the Net Lake-Maybelle River area, northeastern Alberta

Deposition of the Fair Point Formation commenced with shallow lacustrine sedimentation in fault-controlled paleovalleys that were subsequently infilled with locally derived pebble conglomerate. The overlying Manitou Falls Formation consists of a ... Show Abstract

Post, Ryan  2004-12-01

ESR 2001-05

Major- and Trace- Element Geochemistry of Kimberlitic Rocks in Northern Alberta

Samples from the Mountain Lake pipes and the Buffalo Head Hills and Birch Mountains fields contain low SiO2 and Na2O/K2O, with Cr, Ni, MgO, rare-earth elements (REE), Zr and Nb concentrations elevated relative to their abundance in common crustal ... Show Abstract

Eccles, D.R.  Luth, R.W.  2003-05-01

ESR 1981-01

Guidebook for use with soil survey reports of Alberta provincial parks and recreation areas

Outdoor recreation areas must be designed for use without undue deterioration of soil, vegetation, and water resources. Pertinent soil and landscape characteristics need to be recognized.Soil surveys provide for the systematic examination of soils ... Show Abstract

Greenlee, G.M.  1983-01-01

ESR 2004-01

Sequence stratigraphy and its use for uranium exploration in the western Athabasca Basin of Alberta and Saskatchewan

[...]the overlying Lower and Upper Wolverine Point sequences were probably more widespread beyond the present-day margins of the Athabasca Basin. The uppermost Locker Lake-Otherside sequence, although not complete, represents a late normal ... Show Abstract

Collier, B.  2005-05-01

ESR 1976-06

Index to Uranium Assessment Reports for Quartz Mineral Exploration Permits, Northeastern Alberta

Index to Uranium Assessment Reports for Quartz Mineral Exploration Permits, Northeastern Alberta The body of this report is a reproduction of the computer printout of a selective retrieval from the CIGD file, prepared by the Canada Centre for ... Show Abstract

Poruks, M.  Hamilton, W.N.  1976-01-01

ESR 1977-03

Index to Geological, bedrock topography, soils, and groundwater maps of Alberta

The Alberta Research Council; the Geological Survey of Canada (Department of Energy, Mines and Resources, Ottawa); the Research Branch, Canada Department of Agriculture; and the Resource Capability Group, Alberta Energy and Natural Resources are the ... Show Abstract

Root, J.D.  1978-01-01

ESR 1978-03

Geology of the Fort Chipewyan District, Alberta

The geology of 432 square miles (1110 square km) of Precambrian Shield in northeastern Alberta is presented on four map sheets at a scale of 2 inches to 1 mile. A late Hudsonian retrograde greenschist facies metamorphism affected all Shield rocks ... Show Abstract

Godfrey, J.D.  1980-01-01

ESR 2000-02

Distribution and thickness of salt within the Devonian Elk Point Group, Western Canada Sedimentary Basin

Data processing and the application of mapping software resulted in the refinement of the some of the salt boundaries and the production of basin-scale depth to, structure, and isopach maps for the Elk Point salt units. Furthermore, available ... Show Abstract

Grobe, M.  2000-01-01