OCCURRENCE AND RESERVES in C#

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41 OCCURRENCE AND RESERVES
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Tar sand deposits are widely distributed throughout the world in a variety of countries The various tar sand deposits have been described as belonging to two types: (a) materials that are found in stratigraphic traps, and (b) deposits that are located in structural traps There are, inevitably, gradations, and combinations of these two types of deposits and a broad pattern of deposit entrapment are believed to exist The distinction between a structural trap (the usually description of a petroleum reservoir) and a stratigraphic trap is often not clear For example, an anticlinal trap may be related to an underlying buried limestone reef Beds of sandstone may wedge out against an anticline because of depositional variations or intermittent erosion intervals Salt domes, formed by flow of salt at substantial depths, also have created numerous traps that are both a structural trap and a stratigraphic trap In general terms, the entrapment characteristics for the very large tar sand deposits all involve a combination of stratigraphic and structural traps Entrapment characteristics for the very large tar sands all involve a combination of stratigraphic-structural traps There are no very large tar sand accumulations having more than 4 billion barrels in place either in purely structural or in purely stratigraphic traps In a regional sense, structure is an important aspect since all of the very large deposits occur on gently sloping homoclines Furthermore, the tar sand deposits of the world have been described as belonging to two types These are (a) in situ deposits resulting from breaching and exposure of an existing geologic trap and (b) migrated deposits resulting from accumulation of migrating material at outcrop However, there are inevitable gradations and combinations of these two types of deposits The deposits have been laid down over a variety of geologic periods and in different entrapments and a broad pattern of deposit entrapment is believed to exist since all deposits occur along the rim of major sedimentary basins and near the edge of Precambrian shields The deposits either transgress an ancient relief at the edge of the shield
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(eg, those in Canada) or lie directly on the ancient basement (eg, as in Venezuela, West Africa, and Madagascar) A feature of major significance in at least five of the major areas is the presence of a regional cap (usually a widespread transgressive marine shale) Formations of this type occur in the Colorado Group in western Canada, in the Freites formation in eastern Venezuela, or in the Jurassic formation in Melville Island The cap plays an essential role in restraining vertical fluid escape from the basin thereby forcing any fluids laterally into the paleo-delta itself Thus, the subsurface fluids were channeled into narrow outlets at the edge of the basin The potential reserves of hydrocarbon liquids (available through conversion of the bitumen to synthetic crude oil) that occur in tar sand deposits have been variously estimated on a world basis to be in excess of 3 trillion barrels However, the issue is whether or not these reserves can be recovered and conversed to synthetic crude oil Geographic and geologic feature may well put many of these resources beyond the capabilities of current recovery technology requiring new approaches to recovery and conversion
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411 Canada In Canada, the Athabasca deposit along with the neighbouring Wabasca, and Peace River deposits have been estimated to contain approximately 2 trillion barrels of bitumen The town of McMurray, about 240 miles north east of Edmonton, Alberta lies at the eastern margin of the largest accumulation in the world that is, in effect, three major accumulations within the Lower Cretaceous deposits The McMurray-Wabasca reservoirs are found toward the base of the formation and are characteristically cross-bedded coarse grit and gritty sandstone that are unconsolidated or cemented by tar; fine-to-medium grained sandstone and silt occur higher in the sequence Bluesky-Gething and Grand Rapids reservoirs are composed of sub-angular quartz and well-rounded chert grains The McMurray-Wabasca tar sand deposit dips at between 5 and 25 ft/mile (15 and 8 m/mile) to the southwest The Bluesky-Gething sands overlie several unconformities between the Mississippian and Jurassic deposits In the context of the Athabasca deposit, inconsistencies arise presumably because of the lack of mobility of the bitumen at formation temperature [approximately 4 C (39 F)] For example, the proportion of bitumen in the tar sand increases with depth within the formation Furthermore, the proportion of the nonvolatile asphaltenes or the nonvolatile asphaltic fraction (asphaltenes plus resins) in the bitumen also increases with depth within the formation that leads to reduced yields of distillate from the bitumen obtained from deeper parts of the formation In keeping with the concept of higher proportions of asphaltic fraction (asphaltenes plus resins), variations (horizontal and vertical) in bitumen properties have been noted previously, as have variations in sulfur, nitrogen, and metals content Obviously, the richer tar sand deposits occur toward the base of the formation However, the bitumen is generally of poorer quality than the bitumen obtained from near the top of the deposit insofar as the proportions of nonvolatile coke-forming constituents (asphaltenes plus resins) are higher (with increased proportions of nitrogen, sulfur, and metals) near the base of the formation
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412 United States The major tar sand deposits of the United States occur within and around the periphery of the Uinta Basin, Utah These include the Sunnyside, Tar Sand Triangle, Peor (PR) Springs, Asphalt Ridge, and sundry other deposits (Table 41) Asphalt Ridge lies on the northeastern
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