Mannville Group | |
---|---|
Stratigraphic range: Early Cretaceous | |
Type | Geological group |
Sub-units | Glauconitic Sandstone, Ostracod Beds, Ellerslie Member, Grand Rapids Formation, Clearwater Formation, McMurray Formation, Waseca Sand, Sparky Sand, General Petroleum Sand, Rex Sand, Lloydminster Sand, Cummings Member, Dina Member, Pense Formation, Cantuar Formation, Success Formation |
Underlies | Colorado Group |
Overlies | Rundle Group, Banff Formation, Wabamun Formation |
Thickness | up to 145 metres (480 ft) [1] |
Lithology | |
Primary | Sandstone |
Other | Shale |
Location | |
Coordinates | 53°18′31″N111°09′15″W / 53.3087°N 111.1541°W |
Region | Alberta, Saskatchewan |
Country | Canada |
Type section | |
Named for | Mannville, Alberta |
Named by | Nauss, 1945 |
The Mannville Group is a stratigraphical unit of Cretaceous age in the Western Canadian Sedimentary Basin.
It takes the name from the town of Mannville, Alberta, and was first described in the Northwest Mannville 1 well by A.W. Nauss in 1945. [2]
The Mannville Group consists of interbedded continental sand and shale in the base, followed by a calcareous sandstone member, marine shale, glauconitic sandstone and salt and pepper sandstone. An additional non-marine sequence is present in north-eastern Alberta.
Bitumen is produced from the McMurray Formation at the Athabasca Oil Sands. Heavy Oil is produced from the Wabiskaw Member of the Clearwater Formation in the Wabasca oil field, and from multiple formations in the Lloydminster and Provost areas in eastern Alberta and western Saskatchewan. Natural gas is extracted from the Ostracod and Glauconite beds in southern Alberta, and light oil is extracted from the Ellerslie Member in central and southern Alberta. Multiple oil fields [3] and gas fields [4] tap into the Manville Group.
Total gas reserves amount to 316799×106 m3 in the Lower Mannville and 644774×106 m3 in the Upper Mannville. [5] Recoverable oil reserves amount to 105.64×106 m3 in the Lower Mannville and 199.20×106 m3 in the Upper Mannville. [6]
The Mannville Group reaches a thickness of 145 feet (40 m) in its type locality. It occurs in the sub-surface in central Alberta, extending east-west from Edmonton to Lloydminster and north-south from the Deep Basin to the United States border. It is present in the sub-surface in west-central and southern Saskatchewan.
The Mannville Group is discomformably overlain by the Joli Fou Formation shale of the Colorado Group. It rests unconformably on the older Paleozoic carbonates.
It is correlated with the lower Blairmore Group in the Canadian Rockies foothills and to the Bullhead Group and the Spirit River Formation of the Fort St. John Group in north-western Alberta. It is also equivalent to the Cantuar Formation in Saskatchewan and the Swan River Formation in Manitoba.
The Mannville Group includes the following sub-units:
Subdivision | Sub-unit | Age | Lithology | Max Thickness | Reference |
---|---|---|---|---|---|
Upper | Upper Mannville | marine shale and sandstone | |||
Glauconitic Sandstone | Early Cretaceous | very fine to medium grained quartz sandstone with siderite and glauconite | 35 m (110 ft) | [7] | |
Lower Mannville | |||||
Ostracod Beds | Early Cretaceous | Unit A: shale and fossiliferous limestone Unit B: argillaceous limestone with ostracod fossils Unit C: dark shale with siltstone and sandstone interbed Unit D: fine to medium grained lithic calcareous sandstone with kaolinite and chert | 40 m (130 ft) | [8] | |
Ellerslie Member | Early Cretaceous | Upper: fine grained sand with sandy shale and shaley sand lenses Lower: medium grained quartz sand, siltstone, coal | 40 m (130 ft) 30 m (100 ft) | [9] | |
Detrital Beds | Early Cretaceous | Chert pebbles, lithic sandstone, shale, siltstone | 70 m (230 ft) | [10] | |
Sub-unit | Age | Lithology | Max Thickness | Reference |
---|---|---|---|---|
Grand Rapids Formation | Albian | bitumenous fine to medium sand (A, B and C sands, separated by silt and shale) | 125 m (410 ft) | [11] |
Clearwater Formation | Albian | black and green shales and sand | 85 m (280 ft) | [12] |
Wabiskaw Member | Albian | glauconitic sands with black fissile shale | 35 m (110 ft) | [13] |
McMurray Formation | late Barremian to Aptian | fine grained bituminous sands | 60 m (200 ft) | [14] |
Sub-unit | Age | Lithology | Max Thickness | Reference |
---|---|---|---|---|
Colony Sand | Early Cretaceous | friable glauconitic and argillaceous sandstone | 15 m (50 ft) | [15] |
McLaren Member | Early Cretaceous | very fine grained sandstone and shale | 18 m (60 ft) | [16] |
Waseca Sand | Early Cretaceous | sand with silt and shale | 25 m (80 ft) | [17] |
Sparky Sand | Early Cretaceous | sand and shale | 12 m (40 ft) | [18] |
General Petroleum Sand | Early Cretaceous | very fine to fine grained quartzose sand | 15 m (50 ft) | [19] |
Rex Sand | Early Cretaceous | very fine to fine grained quartzose sand with silt and shale | 14 m (50 ft) | [20] |
Lloydminster Sand | Early Cretaceous | unconsolidated quartz sand with silt | 30 m (100 ft) | [21] |
Cummings Member | Early Cretaceous | shale with beds of salt-and-pepper sandstone | 27 m (90 ft) | [22] |
Dina Member | Early Cretaceous | quartz sandstone with siltstone and shale | 60 m (200 ft) | [23] |
Sub-unit | Age | Lithology | Max Thickness | Reference |
---|---|---|---|---|
Pense Formation | Albian | fine grained sandstone, clay, shaly silt | 36 m (120 ft) | [24] |
Cantuar Formation | Aptian to Albian | mudstone and sandstone | 120 m (390 ft) | [25] |
Success Formation | Jurassic to Lower Cretaceous | quartzose sandstone and siltstone | 75 m (250 ft) | [26] |
The Bluesky Formation is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin. It takes the name from the hamlet of Bluesky, and was first described in Shell's Bluesky No. 1 well by Badgley in 1952.
The Cardium Formation is a stratigraphic unit of Late Cretaceous age in the Western Canada Sedimentary Basin. It takes the name from the fossilized heart-shaped cockle shells in the family Cardiidae present. It was first described along the Bow River banks by James Hector in 1895. It is present throughout western Alberta and in northeastern British Columbia, and it is a major source of petroleum and natural gas.
Bullhead Group is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin of northeastern British Columbia and western Alberta. It was first defined by F.H. McLearn in 1918 as the Bullhead Mountain Formation, but later was upgraded to group status. It consists of the Cadomin and Gething Formations, although some early workers included the Bluesky Formation and others in the group.
The Fernie Formation is a stratigraphic unit of Jurassic age. It is present in the western part of the Western Canada Sedimentary Basin in western Alberta and northeastern British Columbia. It takes its name from the town of Fernie, British Columbia, and was first defined by W.W. Leach in 1914.
The Fort St. John Group is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin. It takes the name from the city of Fort St. John, British Columbia and was first defined by George Mercer Dawson in 1881.
The Spirit River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin.
The Smoky Group is a stratigraphical unit of Late Cretaceous age in the Western Canadian Sedimentary Basin.
The Clearwater Formation is a stratigraphic unit of Early Cretaceous (Albian) age in the Western Canada Sedimentary Basin in northeastern Alberta, Canada. It was first defined by R.G. McConnell in 1893 and takes its name from the Clearwater River near Fort McMurray.
The McMurray Formation is a stratigraphic unit of Early Cretaceous age of the Western Canada Sedimentary Basin in northeastern Alberta. It takes the name from Fort McMurray and was first described from outcrops along the banks of the Athabasca River 5 kilometres (3.1 mi) north of Fort McMurray by F.H. McLearn in 1917. It is a well-studied example of fluvial to estuarine sedimentation, and it is economically important because it hosts most of the vast bitumen resources of the Athabasca Oil Sands region.
Colorado is a geologic name applied to certain rocks of Cretaceous age in the North America, particularly in the western Great Plains. This name was originally applied to classify a group of specific marine formations of shale and chalk known for their importance in Eastern Colorado. The surface outcrop of this group produces distinctive landforms bordering the Great Plains and it is a significant feature of the subsurface of the Denver Basin and the Western Canadian Sedimentary Basin. These formations record important sequences of the Western Interior Seaway. As the geology of this seaway was studied, this name came to be used in states beyond Colorado but later was replaced in several of these states with more localized names.
The Ellerslie Member is a stratigraphic unit of Early Cretaceous age in the Western Canadian Sedimentary Basin.
The Alberta Group is a stratigraphical unit of Cenomanian to early Campanian age in the Lewis overthrust in the Western Canadian Sedimentary Basin.
The Exshaw Formation is a stratigraphic unit in the Western Canada Sedimentary Basin. It takes the name from the hamlet of Exshaw, Alberta in the Canadian Rockies, and was first described from outcrops on the banks of Jura Creek north of Exshaw by P.S. Warren in 1937. The formation is of Late Devonian to Early Mississippian age as determined by conodont biostratigraphy, and it straddles the Devonian-Carboniferous boundary.
The Doig Formation is a geologic formation of middle Triassic age in the Western Canadian Sedimentary Basin. It takes the name from Doig River, a tributary of the Beatton River, and was first described in the Texaco N.F.A. Buick Creek No. 7 well by J.H. Armitage in 1962..
The Joli Fou Formation is a allostratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin. It takes the name from the Joli Fou Rapids on the Athabasca River, and was first described in an outcrop along the river, 8 kilometers (5.0 mi) downstream from Joli Fou Rapids, by RTD Wickenden in 1949.
The Woodbend Group is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin.
The Three Forks Group is a stratigraphical unit of Famennian age in the Williston Basin.
The Ellis Group is a stratigraphical unit of Bajocian-Oxfordian age in Alberta, Saskatchewan, Montana and Wyoming in the Western Canadian Sedimentary Basin. It takes the name from Fort Ellis, Montana, and was first described in outcrop in the Rocky Creek Canyon by A.C. Peale in 1893.
The Vanguard Formation is a stratigraphical unit of Callovian to Oxfordian age in the Western Canadian Sedimentary Basin.
The Cenovus Lloydminster Refinery is an asphalt refinery located in the city of Lloydminster, Alberta, Canada owned by Husky Energy. The refinery provides oil products, primarily 30 different grades of asphalt, as well as light distillate, kerosene distillate, atmospheric gas oil, light vacuum gas oil (VGO), and heavy vacuum gas oil. This refinery is Canada's largest asphalt supplier, processing 27,000 barrels of heavy crude oil per day to produce asphalt. Husky is the "largest marketer of paving asphalt in Western Canada with a 29 mbbls/day capacity asphalt refinery located at Lloydminster, Alberta "integrated with the local heavy oil production, transportation and upgrading infrastructure."