Purcell Supergroup
The Purcell Supergroup is composed primarily of argillites, carbonate rocks, quartzites, and mafic igneous rocks of late Precambrian (Mesoproterozoic) age. It is present in an area of about 15,000 km2 (5,800 sq. mi.) in southwestern Alberta and southeastern British Columbia, Canada, and it extends into the northwestern United States where it is called the Belt Supergroup. It was named for the Purcell Mountains of British Columbia by R.A. Daly in 1912.[2] Fossil stromatolites and algal structures are common in some of the Purcell Supergroup rocks,[3][4] and the Sullivan ore body at Kimberley, British Columbia, a world-class deposit of lead, zinc, and silver, lies within the Alderidge Formation in the lower part of the Purcell.[5]
| Purcell Supergroup | |
|---|---|
| Stratigraphic range: | |
| Type | Geological supergroup |
| Sub-units | Many |
| Underlies | Windermere Supergroup |
| Overlies | Canadian Shield |
| Area | 15,000 km2 (5,800 sq. mi.) |
| Thickness | more than 10,000 m (3,200 ft)[1] |
| Lithology | |
| Primary | Argillite, dolomite, quartzite |
| Other | Limestone, igneous rocks |
| Location | |
| Region | Alberta British Columbia |
| Country | Canada |
| Type section | |
| Named for | Purcell Mountains |
| Named by | R.A. Daly, 1912.[2] |
Spectacular outcrops of Purcell and Belt Supergroup rocks can be seen in Glacier National Park in northwestern Montana[6] and Waterton Lakes National Park in southwestern Alberta.[7]
Stratigraphy and lithology edit
The Purcell Supergroup consists primarily of argillites, carbonate rocks (limestone and dolomite), and quartzites, and includes localized occurrences of igneous rocks (mafic lava flows, tuffs, pillow basalts, and gabbroic and dioritic sills and dykes). Sedimentary structures are well preserved in the Purcell rocks despite their great age.[1]
In the southern Canadian Rockies (Waterton Park area), the supergroup is subdivided as follows:
| Geological unit | Lithology | Environment of Deposition | Maximum Thickness | Reference |
|---|---|---|---|---|
| Roosville Formation | green and grey argillite; dolomitic argillite, siltstone and sandstone; argillaceous and stromatolitic dolomite; mudcracks and ripple marks are common. | shallow marine (peritidal) | 1,300 m (4,270 ft) | [1][8][9] |
| Phillips Formation | red, thin-bedded quartz sandstone; siltstone interbedded with argillite and conglomerate; mudcracks and ripple marks are common. | marginal marine to nonmarine | 200 m (660 ft) | [1][8][9] |
| Gateway Formation | red siltstone and argillite; green argillite; dolomitic argillite; dolomitic sandstone; dolomite; and sandy dolomite; casts of salt crystals, mudcracks, ripple marks, and rip-up clasts are locally abundant. | marginal marine | 1,350 m (4,430 ft) | [1][8][9] |
| Sheppard Formation | light grey dolomite and stromatolitic dolomite; red dolomitic siltstone and sandstone; dolomitic argillite. | shallow marine | 275 m (900 ft) | [1][8][9] |
| Purcell Lava | dark green and reddish green to purple chloritized mafic lava flows, pillow basalts, gabbroic sills and dikes; amygdules of quartz, chlorite, and calcite are common. | shallow marine | 150 m (490 ft) | |
| Siyeh Formation | argillaceous limestone and dolomite; black and green argillite; dolomitic quartzite; stromatolitic dolomite. | marginal marine | 790 m (2,590 ft) | [1][8][9] |
| Appekunny Formation | green and maroon argillite; white, grey, green, and pale red sandstone; quartz-pebble conglomerate. | marginal marine | 1,000 m (3,280 ft) | [1][8][9] |
| Altyn Formation | grey, thin-bedded argillaceous limestone and dolomite; massive sandy dolomite and stromatolitic dolomite; dark grey to black argillite. | shallow marine | 300 m (980 ft) | [1][8][9] |
| Waterton Formation | grey, green and red argillaceous dolomite; banded and streaked limestone and dolomite; grey and green, thin-bedded argillite. | marine | 250 m (820 ft) | [1][8][9] |
| Tombstone Mountain Formation | dark grey argillite; dolomitic argillite; argillaceous dolomite and limestone. | marine | 175 m (570 ft) | [1][8][9] |
| Haig Brook Formation | light colored, cliff-forming sequence of dolomite; banded and streaked limestone and dolomite; minor argillite; base of formation is not exposed. | marine | 145 m (480 ft) | [1][8][9] |
In the southern Purcell Mountains (Cranbrook area), the supergroup is subdivided as follows:
| Geological unit | Lithology | Environment of Deposition | Maximum Thickness | Reference |
|---|---|---|---|---|
| Roosville Formation | dolomitic argillite; siltstone; sandstone; and argillaceous and stromatolitic dolomite. | intertidal | 300 m (980 ft) | [4] |
| Phillips Formation | red, thin-bedded quartz sandstone; siltstone interbedded with argillite; ripple marks and mud cracks are abundant locally. | shallow water to subaerial | 150 m (490 ft) | [4] |
| Gateway Formation | grey-green, red, and purple siltstone; dolomitic siltstone; minor interbeds of argillite; casts of salt crystals, mudcracks, ripple marks, and rip-up clasts are locally abundant. | lagoonal | 1,350 m (4,430 ft) | [4] |
| Sheppard Formation | light grey stromatolitic dolomite, interbedded with dolomitic siltstone and argillite; stromatolite mounds up to 10 m (30 ft) thick; mudcracks, ripple marks, and rip-up clasts are locally abundant; casts of salt crystals are rare. | intertidal | 125 m (410 ft) | [4] |
| Intrusive rocks | fine- to coarse-grained sills and dikes of gabbro and diorite intrude the Aldridge to Van Creek Formations. | intrusive | ||
| Nichol Creek Formation | green and purple argillite and siltstone; green volcanic sandstone and tuff interlayered with green or maroon, chloritized and sericitized basaltic to andesitic lavas, some with amygdules of quartz and chlorite. | subaerial | 750 m (2,460 ft) | [4] |
| Van Creek Formation | green to purple argillite and siltstone; mud cracks, ripple marks, and rip-up clasts are locally abundant. | intertidal | 420 m (1,380 ft) | [4] |
| Kitchner Formation | calcareous and dolomitic siltstone and argillite; silty dolomite and limestone; minor quartzite. | shallow subtidal (intertidal at base) | 1,900 m (6,230 ft) | [4] |
| Creston Formation | green, grey, and purple siltstone and argillite; mud cracks, ripple marks, and rip-up clasts are locally abundant. | shallow subtidal (intertidal at top) | 2,350 m (7,710 ft) | [4] |
| Aldridge Formation | fine-grained quartzite; argillaceous quartzite; rusty-weathering grey siltstone; dark grey argillite; base of formation not exposed. | marine (subtidal at top) | >4,200 m (13,780 ft) | [4] |
Environment of deposition edit
The Purcell Supergroup was probably deposited in subsiding deltaic to marine environments along the margin of the North American craton,[10] possibly in an intracratonic basin where North America and another landmass were joined in a supercontinent called Columbia/Nuna.[11] Deposition occurred during the Mesoproterozoic era, much of it probably between about 1470 and 1400 Ma (million years) ago.[12][13]
Distribution and thickness edit
In Canada, the Purcell Supergroup is present in an area of about 15,000 km2 (5,800 sq. mi.) that reaches from the southern Purcell Mountains in southeastern British Columbia to the southern Canadian Rockies in the southwestern Alberta.[1] It extends southward into the United States (western Montana, northern Idaho, northwestern Washington, and western Wyoming) where it is called the Belt Supergroup.[14] It reaches a maximum thickness of more than 10,000 metres (32,000 ft) in the Purcell Mountains.[1]
Relationship to other units edit
The Purcell Supergroup is equivalent to the Belt Supergroup of the northwestern United States. The base of the Purcell is not exposed in Canada, but it is inferred to rest unconformably on the Canadian Shield. The Purcell is unconformably overlain by the Neoproterozoic Windermere Supergroup in most areas, or by younger Cambrian or Devonian formations where the Windermere is absent.[1]
Economic resources edit
The now-closed Sullivan Mine at Kimberley, British Columbia, worked a world-class sedimentary exhalative (SedEx) deposit that is hosted in the lower part of the Purcell Supergroup. During the life of the mine, the Sullivan ore body is reported to have yielded 8,412,077 tons of lead, 7,944,446 tons of zinc, and 9,264 tons of silver, as well as significant quantities of tin and other metals.[5]
References edit
- ^ a b c d e f g h i j k l m n o p 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.
- ^ a b Daly, R.A. 1912. Geology of the North American Cordillera at the Forty-ninth parallel. Geological Survey of Canada, Memoir 38, p. 119-136.
- ^ O'Connor, M.P. 1972. Classification and environmental interpretation of the cryptalgal organosedimentary "Molar-Tooth" structure from the Late Precambrian Belt-Purcell Supergroup. Journal of Geology, vol. 80, no. 5, p. 592-610.
- ^ a b c d e f g h i j k McMechan, M.E. 1981. The Middle Proterozoic Purcell Supergroup in the southwestern Rocky and southeastern Purcell Mountains, British Columbia, and the initiation of the Cordilleran Miogeocline, southern Canada and adjacent United States. Bulletin of Canadian Petroleum Geology, vol. 29, no. 4, p. 583-621.
- ^ a b Lydon, John W. "Geology and metallogeny of the Belt-Purcell Basin. In: Goodfellow, W.D. (ed.), Mineral deposits of Canada: a synthesis of major deposit types, district metallogeny, the evolution of geological provinces, and exploration methods. Geological Association of Canada, Mineral Deposits Division, Special Publication no. 5, p. 581-607". Retrieved 29 April 2018.
- ^ Alt, D.D. and Hyndman, D.W. 1986. Roadside geology of Montana. Mountain Press Publishing Co., Missoula, Montana, 427 p. ISBN 0-87842-202-1,
- ^ Gordy, P.L., Frey, F.R. and Norris, D.K. 1977. Geological guide for the CSPG 1977 Waterton-Glacier Park Field Conference. Canadian Society of Petroleum Geologists, Calgary, Alberta, 93 p.
- ^ a b c d e f g h i j k Prior, G. J., Hathaway, B., Glombick, P.M., Pana, D.I., Banks, C.J., Hay, D.C., Schneider, C.L., Grobe, M., Elgr, R., and Weiss, J.A. (2013). . Archived from the original on 2016-06-26. Retrieved 2016-06-20.
{{cite web}}: CS1 maint: multiple names: authors list (link) - ^ a b c d e f g h i j k Alberta Geological Survey, 2013. . Archived from the original on 1 May 2018. Retrieved 1 May 2018.
{{cite web}}: CS1 maint: numeric names: authors list (link) - ^ Hein, F.J. and McMechan, M.E. 1994. "Atlas of the Western Canada Sedimentary Basin (Mossop, G.D. and Shetsen, I., compilers), Chapter 6: Proterozoic and Lower Cambrian strata of the Western Canada Sedimentary Basin". Retrieved 11 April 2018.
{{cite web}}: CS1 maint: multiple names: authors list (link) CS1 maint: numeric names: authors list (link) - ^ Schieber, J., 1989. The origin of the Neihart Quartzite, a basal deposit of the mid-Proterozoic Belt Supergroup, Montana, USA. Geological Magazine, v. 126, p. 271-281.
- ^ Evans, K.V., Aleinikoff, J.N., Obradovich, J.D. and Fanning, C.M. 2000. SHRIMP U-Pb geochronology of volcanic rocks, Belt Supergroup, western Montana: evidence for rapid deposition of sedimentary strata. Canadian Journal of Earth Sciences, v. 37, p.1287-1300.
- ^ Halpin, Jacqueline A.; Jensen, Torsten; McGoldrick, Peter; Meffre, Sebastien; Berry, Ron F.; Everard, John L.; Calver, Clive R.; Thompson, Jay; Goemann, Karsten; Whittaker, Joanne M. (2014). "Authigenic monazite and detrital zircon dating from the Proterozoic Rocky Cape Group, Tasmania: Links to the Belt-Purcell Supergroup, North America". Precambrian Research. 250: 50–67. Bibcode:2014PreR..250...50H. doi:10.1016/j.precamres.2014.05.025.
- ^ Lori Tapanila and Paul Link. "Mesoproterozoic Belt Supergroup". Digital Geology of Idaho. Idaho State University, Department of Geosciences. Retrieved 16 September 2016.