Spirit River Formation: Difference between revisions
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{{Infobox |
{{Infobox rockunit |
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| name |
| name = Spirit River Formation |
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| image |
| image = FalherMBR.JPG |
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| caption |
| caption = Falher graywake and shale |
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| type |
| type = [[Geological formation]] |
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| age |
| age = {{Fossil range|Albian|Albian|middle [[Albian]]}} |
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| prilithology |
| prilithology = [[sandstone]], [[shale]], [[siltstone]] |
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| otherlithology = [[coal]], [[ironstone]], [[greywacke]] |
| otherlithology = [[coal]], [[ironstone]], [[greywacke]] |
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| namedfor |
| namedfor = [[Spirit River (Alberta)|Spirit River]] |
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| namedby |
| namedby = Badgley, 1952 |
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| region |
| region = {{flag|Alberta}}, {{flag|British Columbia}} |
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| country |
| country = {{flag|Canada}} |
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| coordinates |
| coordinates = {{coord|55.775|N|118.906|W|name=Imperial Spirit River No. 1 well, in 12-20-78-6W6M|display=inline,title}} |
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| unitof |
| unitof = [[Fort St. John Group]] |
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| subunits |
| subunits = Notikewin Member, Falher Member, Wilrich Member |
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| underlies |
| underlies = [[Peace River Formation]] |
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| overlies |
| overlies = [[Bluesky Formation]] |
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| thickness |
| thickness = up to {{convert|348|ft|m|-1}}<ref name=lexicon>{{Cite web | url = http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011614 | title = Peace River Formation | author = [[Lexicon of Canadian Geologic Units]] | accessdate = 2009-02-11}}</ref> |
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| extent = |
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| area = |
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| map = |
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| map_caption = |
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}} |
}} |
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The '''Spirit River Formation''' is a [[Stratigraphy|stratigraphical]] unit of middle [[Albian]] [[Geochronology|age]] in the [[Western Canadian Sedimentary Basin]]. |
The '''Spirit River Formation''' is a [[Stratigraphy|stratigraphical]] unit of middle [[Albian]] [[Geochronology|age]] in the [[Western Canadian Sedimentary Basin]]. |
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It takes the name from the |
It takes the name from the [[Spirit River (Alberta)|Spirit River]], and was first described in [[Imperial Oil]] Spirit River No. 1 well by Badgley in 1952.<ref>Badgley, Peter C., 1952. Notes on the subsurface stratigraphy and oil and gas geology of the Lower Cretaceous series in central Alberta (Report and seven figures); [[Geological Survey of Canada]], Paper No. 52-11, 12 p.</ref> |
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==Lithology== |
==Lithology== |
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The Spirit River Formation consists, from bottom to top of fine to medium grained argillaceous [[sandstone]], dark [[shale]], [[ironstone]], [[greywacke]], [[shale]], [[siltstone]], [[coal]] and dark [[shale]] with thin [[sandstone]] and [[siltstone]] stringers.<ref name=lexicon/> |
The Spirit River Formation consists, from bottom to top of fine to medium grained argillaceous [[sandstone]], dark [[shale]], [[ironstone]], [[greywacke]], [[shale]], [[siltstone]], [[coal]] and dark [[shale]] with thin [[sandstone]] and [[siltstone]] stringers.<ref name=lexicon/> |
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=== |
===Hydrocarbon production=== |
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[[Natural gas|Gas]] is produced from [[channels]] developed in the [[Falher Member]] in northern [[Alberta]]. |
[[Natural gas|Gas]] is produced from [[Channel (geography)|channels]] developed in the [[Falher Member]] in northern [[Alberta]]. |
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==Hydraulic fracturing in Canada== |
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{{main|Hydraulic fracturing in Canada}} |
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'Massive' hydraulic fracturing has been widely used in [[Alberta]] since the late 1970s to recover gas from low-permeability sandstones of the Spirit River Formation.<ref>{{cite journal | first1 = Douglas J. | last1 = Cant | first2 = Valerie G. | last2 = Ethier | title = Lithology-dependent diagenetic control of reservoir properties of conglomerates, Falher member, Elmworth Field, Alberta | journal = Bulletin of the [[American Association of Petroleum Geologists]] | date = August 1984 | volume = 68 | number = 8 }}</ref>{{rp|1044}} Massive hydraulic fracturing has been widely used in [[Alberta]] since the late 1970s. The method is currently used in development of the [[Cardium Formation|Cardium]], [[Duvernay Formation|Duvernay]], [[Montney Formation|Montney]] and [[Viking Formation|Viking]] formations in [[Alberta]], [[Bakken Formation|Bakken]] formation in [[Saskatchewan]], [[Montney Formation|Montney]] and [[Horn River Formation|Horn River]] formations in [[British Columbia]]. |
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==Distribution== |
==Distribution== |
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The |
The Spirit River Formation reaches a maximum thickness of {{convert|348|m|ft|-1}}. It is found in the sub-surface in the [[Peace River Country]], in an area stretching from [[Fort St. John, British Columbia]] to the [[Lesser Slave Lake]] from west to east, and from [[Grande Prairie, Alberta]] to [[Manning, Alberta]] from south to north. |
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==Relationship to other units== |
==Relationship to other units== |
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The Spirit River Formation is conformably overlain by the [[Peace River Formation]] and conformably underlain by the [[Bluesky Formation]]. It grades laterally to the [Buckinghorse Formation]] shales to the north-east, and into the sandy [[facies]] of the [[Malcolm Creek Formation]] south of the [[Wapiti River]]. It is equivalent to the upper [[Mannville Formation]] in [[Central Alberta]] and to the [[Clearwater Formation]] and [[Grand Rapids Formation]] in the upper [[ |
The Spirit River Formation is conformably overlain by the [[Peace River Formation]] and conformably underlain by the [[Bluesky Formation]]. It grades laterally to the [[Buckinghorse Formation]] shales to the north-east, and into the sandy [[facies]] of the [[Malcolm Creek Formation]] south of the [[Wapiti River]]. It is equivalent to the upper [[Mannville Formation]] in [[Central Alberta]] and to the [[Clearwater Formation]] and [[Grand Rapids Formation]] in the upper [[Athabasca River]] area.<ref name=lexicon/> |
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⚫ | |||
⚫ | |||
The Spirit River Formation is composed of the following sub-divisions from base to top: |
The Spirit River Formation is composed of the following sub-divisions from base to top: |
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{|class="wikitable" |
{|class="wikitable" |
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! [[Geological unit|Sub-unit]] !! Lithology !! Max<br>Thickness !! Reference |
! [[Geological unit|Sub-unit]] !! Lithology !! Max<br>Thickness !! Reference |
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|Notikewin Member || fine to medium grained argillaceous [[sandstone]], dark [[shale]], [[ironstone]] || {{convert|28|m|ft|-1}} |
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|<ref>{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011050|title=Notikewin Member|author=Lexicon of Canadian Geologic Units |accessdate=2009-02-11}}</ref> |
|<ref>{{Cite web | url = http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011050 | title = Notikewin Member | author = [[Lexicon of Canadian Geologic Units]] | accessdate = 2009-02-11}}</ref> |
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|Falher Member || [[greywacke]], [[shale]], [[siltstone]], [[coal]] || {{convert|215|m|ft|-1}} |
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|<ref>{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:004811|title=Falher Member|author=Lexicon of Canadian Geologic Units |accessdate=2009-02-11}}</ref> |
|<ref>{{Cite web | url = http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:004811 | title = Falher Member | author = [[Lexicon of Canadian Geologic Units]] | accessdate = 2009-02-11}}</ref> |
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|Wilrich Member || dark [[shales]] thin [[sandstone]] and [[siltstone]] stringers || {{convert|154|m|ft|-1}} |
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|<ref>{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:016545 |title=Wilrich Member|author=Lexicon of Canadian Geologic Units |accessdate=2009-02-11}}</ref> |
|<ref>{{Cite web | url = http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:016545 | title = Wilrich Member | author = [[Lexicon of Canadian Geologic Units]] | accessdate = 2009-02-11}}</ref> |
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==References== |
==References== |
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{{reflist}} |
{{reflist}} |
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{{WCSB|Northwest_Plains=yes}} |
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[[Category: |
[[Category:Geologic formations of Alberta]] |
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[[Category: |
[[Category:Geologic formations of British Columbia]] |
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[[Category:Cretaceous Alberta]] |
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[[Category:Cretaceous British Columbia]] |
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{{geology-stub}} |
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[[Category:Sandstone formations of Canada]] |
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[[Category:Shale formations]] |
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[[Category:Siltstone formations]] |
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[[Category:Coal formations]] |
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[[Category:Western Canadian Sedimentary Basin]] |
Latest revision as of 00:51, 17 July 2024
Spirit River Formation | |
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Stratigraphic range: | |
Type | Geological formation |
Unit of | Fort St. John Group |
Sub-units | Notikewin Member, Falher Member, Wilrich Member |
Underlies | Peace River Formation |
Overlies | Bluesky Formation |
Thickness | up to 348 feet (110 m)[1] |
Lithology | |
Primary | sandstone, shale, siltstone |
Other | coal, ironstone, greywacke |
Location | |
Coordinates | 55°46′30″N 118°54′22″W / 55.775°N 118.906°W |
Region | Alberta, British Columbia |
Country | Canada |
Type section | |
Named for | Spirit River |
Named by | Badgley, 1952 |
The Spirit River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin.
It takes the name from the Spirit River, and was first described in Imperial Oil Spirit River No. 1 well by Badgley in 1952.[2]
Lithology
[edit]The Spirit River Formation consists, from bottom to top of fine to medium grained argillaceous sandstone, dark shale, ironstone, greywacke, shale, siltstone, coal and dark shale with thin sandstone and siltstone stringers.[1]
Hydrocarbon production
[edit]Gas is produced from channels developed in the Falher Member in northern Alberta.
Hydraulic fracturing in Canada
[edit]'Massive' hydraulic fracturing has been widely used in Alberta since the late 1970s to recover gas from low-permeability sandstones of the Spirit River Formation.[3]: 1044 Massive hydraulic fracturing has been widely used in Alberta since the late 1970s. The method is currently used in development of the Cardium, Duvernay, Montney and Viking formations in Alberta, Bakken formation in Saskatchewan, Montney and Horn River formations in British Columbia.
Distribution
[edit]The Spirit River Formation reaches a maximum thickness of 348 metres (1,140 ft). It is found in the sub-surface in the Peace River Country, in an area stretching from Fort St. John, British Columbia to the Lesser Slave Lake from west to east, and from Grande Prairie, Alberta to Manning, Alberta from south to north.
Relationship to other units
[edit]The Spirit River Formation is conformably overlain by the Peace River Formation and conformably underlain by the Bluesky Formation. It grades laterally to the Buckinghorse Formation shales to the north-east, and into the sandy facies of the Malcolm Creek Formation south of the Wapiti River. It is equivalent to the upper Mannville Formation in Central Alberta and to the Clearwater Formation and Grand Rapids Formation in the upper Athabasca River area.[1]
Subdivisions
[edit]The Spirit River Formation is composed of the following sub-divisions from base to top:
Sub-unit | Lithology | Max Thickness |
Reference |
---|---|---|---|
Notikewin Member | fine to medium grained argillaceous sandstone, dark shale, ironstone | 28 metres (90 ft) | [4] |
Falher Member | greywacke, shale, siltstone, coal | 215 metres (710 ft) | [5] |
Wilrich Member | dark shales thin sandstone and siltstone stringers | 154 metres (510 ft) | [6] |
References
[edit]- ^ a b c Lexicon of Canadian Geologic Units. "Peace River Formation". Retrieved 2009-02-11.
- ^ Badgley, Peter C., 1952. Notes on the subsurface stratigraphy and oil and gas geology of the Lower Cretaceous series in central Alberta (Report and seven figures); Geological Survey of Canada, Paper No. 52-11, 12 p.
- ^ Cant, Douglas J.; Ethier, Valerie G. (August 1984). "Lithology-dependent diagenetic control of reservoir properties of conglomerates, Falher member, Elmworth Field, Alberta". Bulletin of the American Association of Petroleum Geologists. 68 (8).
- ^ Lexicon of Canadian Geologic Units. "Notikewin Member". Retrieved 2009-02-11.
- ^ Lexicon of Canadian Geologic Units. "Falher Member". Retrieved 2009-02-11.
- ^ Lexicon of Canadian Geologic Units. "Wilrich Member". Retrieved 2009-02-11.