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Western Canada sedimentary basin

The Cretaceous sedimentary rocks of the Western Canada Sedimentary Basin (WCSB), renowned for their hydrocarbon resources, are seldom considered to have potential to host base metal sulphide mineralization. These sedimentary rocks have also discouraged those who presumed that the Precambrian rocks of the Canadian Shield to the east and north are more favourable hosts of base metal mineralization (ctMacqueen 1997). [Pg.29]

Paradis, S., Turner, W.A., Coniglio, M., Wilson, N. Nelson, J.L. 2006. Stable and radiogenic isotopic signatures of mineralized Devonian carbonates of the Northern Rocky Mountains and the Western Canada Sedimentary Basin. In Hannigan, P.K. (ed) Potential for carbonate-hosted lead-zinc Mississippi Valley-type mineralization in northern Alberta and southern Northwest Territories Geoscience Contributions,... [Pg.32]

The Beaufort-Mackenzie Basin hosts immense unconventional natural gas hydrate reserves that are often co-located with conventional petroleum resources. Osadetz et al. (2005) reported that the conventional resources are co-located with an immense gas hydrate resource estimated between 2.4 x 1012 and 87 x 1012 m3 of raw natural gas. Because the expected decline in conventional natural gas production from the Western Canada Sedimentary Basin cannot be replaced by conventional production from frontier regions alone, this immense hydrate resource offers a solution to replace the expected decline in conventional gas reserves. [Pg.159]

This paper deals with three different proposed protected areas that are in different stages with respect to their NRAs Edehzhie (Horn Plateau), Ts ude niline Tu eyeta (Ramparts), Sambaa K e (Trout Lake). Thus for the three areas different issues and/or stages will be highlighted. All three areas lie (at least partly) within the Western Canada Sedimentary Basin. [Pg.422]

Paulen, R.C., 2009. Sampling techniques in the Western Canada Sedimentary Basin and the Cordillera. In R.C. Paulen I. McMartin (eds.), Application of Till and Stream Sediment Heavy Mineral and Geochemical Methods to Mineral Exploration in Western and Northern Canada, Geological Association of Canada, GAC Short Course Notes 18, 41-59. [Pg.424]

Coleman ML, Sheppard TJ, Durham JJ, Rouse JE, Moore GR (1982) Reduction of water with zinc for hydrogen isotope analysis. Anal Chem 54 993-995 Connolly CA, Walter LM, Baadsgaard H, Longstaffe F (1990) Origin and evolution of formation fluids, Alberta Basin, western Canada sedimentary basin II. Isotope systematics and fluid mixing. Applied Geochem 5 397 14... [Pg.237]

Formation Waters in the Western Canada Sedimentary Basin. 2. Alkali Metals, Chem. Geol. (1969) 4, 211. [Pg.33]

Western Canada Sedimentary Basin between Latitudes 49° and 60°N, Bull. Am. Assoc. Petrol. Geol. (1968) 52, 2318. [Pg.35]

Hitchon, B., "Fluid Flow in Western Canada Sedimentary Basin. 1. [Pg.36]

An interesting implication of the Toth-Freeze-Witherspoon model is the deep penetration of surface water into the basin over geologic time. This has been used to derive a geochemical mass balance model for the mixing of surface water and diagenetically modified sea water in the Western Canada sedimentary basin using deuterium as a tracer (204). [Pg.50]

Sulfur compounds in the gas oil fractions from two bitumens (Athabasca oil sand and Cold Lake deposit)> a heavy oil (Lloydminster) from Cretaceous reservoirs along the western Canada sedimentary basin, and a Cretaceous oil from a deep reservoir that may be mature (Medicine River) are investigated. The gas oil distillates were separated to concentrates of different hydrocarbon types on a liquid adsorption chromatographic column. The aromatic hydrocarbon types with their associated sulfur compounds were resolved by gas chromatographic simulated distillation and then by gas solid chromatography. Some sulfur compounds were further characterized by mass spectrometry. The predominant sulfur compounds in these fractions are alkyl-substituted benzo- and dibenzothiophenes with short side chains which have few dominant isomers. [Pg.16]

Hitchon B. and Friedman I. (1969) Geochemistry and origin of formation waters in the western Canada sedimentary basin I. Stable isotopes of hydrogen and oxygen. Geochim. Cosmochim. Acta 33, 1321-1349. [Pg.2787]

Spencer R. J. (1987) Origins of Ca-Cl brines in Devonian formations, western Canada sedimentary basin. Appl. Geochem. 2, 373-384. [Pg.2830]

Garven, G., 1985. The role of regional fluid flow in the genesis of the Pine Point Deposit, Western Canada Sedimentary Basin. Economic Geology, Vol. 80, pp. 307-324 Garven, G., 1989. A hydrogeologic model for the formation of the giant oil sands deposits of the Western Canada Sedimentary Basin. American Journal of Science, Vol. 289, pp. 105-166... [Pg.257]

Hitchon, B., 1969a. Fluid flow in the western Canada sedimentary basin, 1. Effect of topography. Water Resour. Res., 5(1) 186—195. [Pg.242]

Longstaffe, F.J. (1994) Stable isotopic constraints on sandstone diagenesis in the Western Canada Sedimentary Basin. In Quantitative Diagenesis Recent Developments and Applications to Reservoir Geology (Eds. Parker, A. Sellwood, B.W.), pp. 223-274. Kluwer Academic, Dordrecht. [Pg.161]


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See also in sourсe #XX -- [ Pg.41 ]

See also in sourсe #XX -- [ Pg.7 , Pg.8 , Pg.9 , Pg.10 , Pg.11 , Pg.12 , Pg.13 , Pg.14 , Pg.15 , Pg.16 , Pg.17 , Pg.18 , Pg.19 , Pg.20 , Pg.21 , Pg.22 , Pg.23 , Pg.24 , Pg.25 ]




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Sedimentary basins

Western

Western Canada

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