Gog Group
{{Short description|Stratigraphic unit in the Western Canada Sedimentary Basin}}
{{Infobox rockunit
| name = Gog Group
| image = CambrianRusophycus.jpg
| caption = Trace fossils in a slab from the Gog Group.
| type = Group
| age = {{Fossil range|541|509|Early Cambrian)}}
| period = Cambrian
| prilithology = Quartzose sandstone, quartzite, conglomerate
| otherlithology = Siltstone, mudstone, limestone, dolomite
| namedfor =
| namedby = C.F. Deiss, 1940Deiss, C.F. 1940. Lower and Middle Cambrian stratigraphy of southwestern Alberta and southeastern British Columbia. Geological Society of America Bulletin, vol. 57, p. 731-794.
| region = {{flag|Alberta}} {{flag|British Columbia}}
| country = {{flag|Canada}}
| coordinates =
| unitof =
| subunits = see text
| underlies = Mount Whyte Formation, Chancellor Group, Snake Indian Formation
| overlies = Miette Group
| thickness = up to {{convert|2180|m|ft|-1}}
| extent =
| area =
| map =
| map_caption =
}}
The Gog Group is a stratigraphic unit in the Western Canada Sedimentary Basin. It is present in the eastern and western main ranges of the Canadian Rockies in Alberta and British Columbia.Desjardins, P.R., Buatois, L.A., Pratt, B.E. and Mágano, M.G. 2010. Stratigraphy and sedimentary environments of the Lower Cambrian Gog Group in the southern Rocky Mountains of western Canada. Bulletin of Canadian Petroleum Geology, vol. 58, p. 403-439. It was named by C.F. Deiss in 1940 after Gog Lake near its type locality at Wonder Pass near Mount Assiniboine.Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. {{ISBN|0-920230-23-7}}.
Lithology and environment of deposition
The Gog Group consists primarily of thick deposits of cross-bedded quartzose sandstone and quartzite, with minor quartzitic conglomerate and sub-arkosic sandstone. It also includes mudstone, siltstone, limestone and dolomite formations. The Gog sediments are thought to have been deposited in shallow marine environments on the subsiding margin of the North American craton (Laurentia).Hein, H. J., and M. E. McMechan (1994). [http://ags.aer.ca/reports/atlas-of-the-western-canada-sedimentary-basin.htm Chapter 6 Proterozoic and Lower Cambrian Strata of the Western Canada Sedimentary Basin] {{Webarchive|url=https://web.archive.org/web/20160701131122/http://ags.aer.ca/reports/atlas-of-the-western-canada-sedimentary-basin.htm |date=2016-07-01 }}; in Geological Atlas of the Western Canada Sedimentary Basin, G.D. Mossop and I. Shetsen (comp.). Alberta, Canada: Canadian Society of Petroleum Geologists and Alberta Research Council.[Last accessed 28 June 2016].Hein, F.J. and Arnott, R.W. 1983. Precambrian Miette conglomerates, Lower Cambrian Gog quartzites and modern braided outwash deposits, Kicking Horse Pass area. Canadian Society of Petroleum Geologists Field Trip Guidebook, 1983, 46 p.
Stratigraphy
=Subdivisions=
The Gog Group is subdivided into the following formations:
== [[Jasper, Alberta|Jasper]] area (north) ==
== [[Kicking Horse Pass]] area (south) ==
class="wikitable" | ||||
Formation | Age | Lithology | Max. Thickness | Reference |
---|---|---|---|---|
Peyto Formation | late Early Cambrian | limestone, dolomite | {{convert|125|m|ft | |
1|abbr=on}} | ||||
St. Piran Formation | Early Cambrian | quartzose sandstone | {{convert|825|m|ft | |
1|abbr=on}} | ||||
Lake Louise Formation | Early Cambrian | limestone, dolomite, shale, quartzose sandstone | | | |
Fort Mountain Formation | Early Cambrian | quartzose sandstone, quartzite, arkosic sandstone, conglomerate | {{convert|510|m|ft | |
1|abbr=on}} | ||||
Jasper Formation | Early Cambrian | arkosic sandstone, quartzite, conglomerate, argillite | {{convert|500|m|ft | |
1|abbr=on}} |
Paleontology
Trace fossils such as Skolithos, Cruziana, Diplocraterion, Chondrites, Planolites, Rusophycus and others are abundant in the Gog Group sediments, and Early Cambrian trilobites of the genus Olenellus are found in the Peyto Formation limestones at the top of the Group. Small archaeocyathid bioherms have been reported from the base of the Mahato Formation, and archaeocyathids, salterellids, primitive brachiopods and echinoderms have been reported from the Mural Formation.
See also
{{Portal |Earth sciences|Canada|Paleontology}}
References
{{Reflist}}
{{Western Canadian Sedimentary Basin|Canadian Rockies=yes}}
Category:Western Canadian Sedimentary Basin
Category:Geologic groups of Alberta
Category:Cambrian British Columbia
Category:Geologic groups of British Columbia