Great Falls Tectonic Zone
The Great Falls Tectonic Zone is a major intracontinental shear zone between the Hearne craton and Wyoming craton basement rock of the Archean Eon which form part of the North American continent.[1][2][3][4][5] The zone is an area about 100 miles (150 km) wide extending from the southwestern Idaho-Montana border across Montana to the northwestern Montana-Saskatchewan-North Dakota border.[4][6] It is named for the Great Falls of the Missouri River, a major geologic feature of the area. The central and western portions of the zone are believed to be about 1.1 to 3.3 billion years old.[7] The central part of the zone lacks Archean rock, however, leading at least one group of scientists to speculate that it was formed very late in the Paleoproterozoic Era.[7]
The Great Falls tectonic zone has been periodically active since the Proterozoic, and possibly as late as the Holocene.[6] Little of the zone is visible due to Phanerozoic cover, the exception being the Little Belt Mountains.[2] However, it is believed that the tectonic zone controlled the geologic development of nearby basins and subbasins.[8]
The Great Falls tectonic zone was first identified in 1985.[4] Geologists originally believed the zone was part of the Wyoming craton, but now conclude that it is distinct from it.[2] There is continuing controversy over whether the region is a shear zone or suture,[1][9] and the role the zone played in the formation of the North American continent.[2] At one time, both the Great Falls Tectonic Zone and the Vulcan structure were both considered sutures, but debate remains open on the point.[2] At least one group of geologists has concluded the zone represents the closure of an ocean basin.[2] The zone lacks gravity anomalies or electromagnetic signatures which would allow scientists to conclude that it was generated by subduction.[4] There is significant evidence that the zone has been periodically remineralized since Precambrian times.[10] Square Butte, Shaw Butte, Crown Butte and the other structures of the Adel Mountains Volcanic Field lie astride the tectonic zone near the city of Great Falls.[11]
See also
References
- ↑ 1.0 1.1 Boerner, D.E.; Craven, J.A.; Kurtz, R.D.; Ross, G.M.; and Jones, F.W. "The Great Falls Tectonic Zone: Suture or Intracontinental Shear Zone?" Canadian Journal of Earth Sciences. 35:2 (1998).
- ↑ 2.0 2.1 2.2 2.3 2.4 2.5 Mueller, Paul A.; Heatherington, Ann L.; Kelly, Dawn M.; Wooden, Joseph L.; and Mogk, David W. "Paleoproterozoic Crust Within the Great Falls Tectonic Zone: Implications for the Assembly of Southern Laurentia." Geology. 30:2 (February 2002).
- ↑ O'Neill, J. Michael and Lo, David A. "Character and Regional Significance of Great Falls Tectonic Zone, East-Central Idaho and West-Central Montana." AAPG Bulletin. 69 (1985).
- ↑ 4.0 4.1 4.2 4.3 Harms, Tekla A.; Brady, John B.; Burger, H. Robert; and Cheney, John T. "Advances in the Geology of the Tobacco Root Mountains, Montana, and Their Implications for the History of the Northern Wyoming Province." Precambrian Geology of the Tobacco Root Mountains, Montana. Special Papers, Volume 377. John B. Brady, H. Robert Burger, John T. Cheney, and Tekla A. Harms, eds. Boulder, Colo.: Geological Society of America, 2004. ISBN 0-8137-2377-9
- ↑ Rogers, John James William and Santosh, M. Continents and Supercontinents. New York: Oxford University Press, 2004. ISBN 0-19-516589-6
- ↑ 6.0 6.1 O'Neill, J. Michael and Lopez, David A. "Character and Regional Significance of the Great Falls Tectonic Zone, East-Central Idaho and West-Central Montana." American Association of Petroleum Geologists Bulletin. 69:3 (1985).
- ↑ 7.0 7.1 Gifford, Jennifer N.; Foster, David A.; Mueller, Paul A.; Mogk, D.W.; Kamenov, George D.; and Probst, Kelly. Plutonic Imaging: A View into the Lower Crust and Upper Mantle of the Great Falls Tectonic Zone. 2008 Joint GSA, SSSA-ASA-CSSA, and GCAGS Annual Meeting. October 7, 2008.
- ↑ O'Neill, J.M., editor. Metallogeny of Mesoproterozoic Sedimentary Rocks in Idaho and Montana—Studies by the Mineral Resources Program, 2004–2007. U.S. Geological Survey Open-File Report 2007–1280. Washington, D.C.: U.S. Geological Survey, 2007.
- ↑ Sears, James W.; Harms, Tekla A.; and Evenchick, C.A. Whence the Mountains?: Inquiries Into the Evolution of Orogenic Systems: A Volume in Honor of Raymond A. Price. Boulder, Colo.: Geological Society of America, 2007. ISBN 0-8137-2433-3
- ↑ Foster, F. and Childs, J.F. "An Overview of Significant Gold Lode Systems in Montana, and Their Regional Geologic Setting." Explorations in Mining Geology. 2 (1993); Hoy, T. "The Purcell Supergroup in Southeastern British Columbia: Sedimentation, Tectonics and Stratiform Lead-Zinc Deposits." In Precambrian Sulfide Deposits. Special Paper 25. Geological Association of Canada, 1982.
- ↑ Hearn Jr., B. Carter. "The Homestead Kimberlite, Central Montana, USA: Mineralogy, Xenocrysts, and Upper-Mantle Xenoliths." Lithos. 77:1-4 (September 2004); Alt, David and Hyndman, Donald W. Northwest Exposures: A Geologic Story of the Northwest. Missoula, Mont.: Mountain Press, 1995. ISBN 0-87842-323-0
