The Illinois Basin is a Paleozoic depositional and structural basin in the United States, centered in and underlying most of the state of Illinois, and extending into southwestern Indiana and western Kentucky. The basin is elongate, extending approximately 400 miles northwest-southeast, and 200 miles southwest-northeast.
Boundaries and sedimentary rocks
The basin is bordered on the northeast by the Kankakee Arch, on the southeast by the Cincinnati Arch, on the south by the Pascola Arch, on the southwest by the Ozark Dome, on the northwest by the Mississippi River Arch, and on the north by the Wisconsin Arch. The New Madrid Seismic Zone and the Wabash Valley Seismic Zone intersect the southern portion of the basin.
At its center beneath southern Illinois, the basin contains a thickness of about 15,000 feet of Cambrian through Pennsylvanian sedimentary rocks, predominantly marine, and mostly dolomite, limestone, shale, and sandstone.
Bituminous coal is present in Pennsylvanian rocks in the basin, deposited in freshwater swamp environments. Over the years, the Illinois Basin has produced more than eight billion tons of coal in Southern Illinois, particularly in the Harrisburg Coal Field, and the Western Coal Fields of Kentucky. Coal production was 99 million short tons in 2008, roughly equally divided between Illinois, Indiana, and western Kentucky. The basin provided 8% of US coal production in 2008.
The Illinois Basin has produced more than four billion barrels of petroleum. Major oil production began in 1905, and from 1907 through 1912, the basin was the third-most oil productive area in the United States. Oil production peaked in 1908 at 34 million barrels per year, and declined steadily to 5 million barrels in 1933. A new wave of exploration brought oil production to a new high of 140 million barrels in 1940, after which production again declined. Waterflooding of old reservoirs caused a third peak of oil production in the 1950s.
The rocks of the Illinois Basin are thought to be the source of metals in Mississippi Valley-Type lead-zinc deposits, both within the basin and in surrounding areas, such as the Lead Belt of southeast Missouri.
Within the basin, deposits valuable for lead, zinc, coal balls and fluorite are mined in Hardin and Pope counties, Illinois, and Crittenden and Livingston counties, Kentucky. the deposits are in the form of veins and limestone replacement deposits in Mississippian sedimentary rocks. Ore minerals are fluorite, galena, and sphalerite. Gangue minerals include common quartz and calcite, and minor barite and chalcopyrite.
Some geologic formations in the Illinois Basin are considered to have potential for carbon sequestration, as a permanent disposal site for carbon dioxide that would otherwise be released into the atmosphere. In 2009, Archer Daniels Midland Corp. began pilot testing the carbon sequestration potential of the Mt. Simon formation beneath its ethanol manufacturing facility in Illinois. As of January 2015, one million metric tons of carbon dioxide had been sequestered in the Illinois Basin-Decatur Project.
- GA Mansoori, N Enayati, LB Agyarko (2016), Energy: Sources, Utilization, Legislation, Sustainability, Illinois as Model State, World Sci. Pub. Co., ISBN 978-981-4704-00-7
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- Robert M. Grogan and James C. Bradbury, "Fluorite-zinc-lead deposits of the Illinois-Kentucky mining district," in Ore Deposits in the United States, New York: American Institute of Mining, Metallurgical, and Petroleum Engineers (AIME), 1968, v.1, p.370-399.
- Archer Daniels Midland, Carbon-sequestration projects put innovative emissions-reduction technology to the test, accessed 26 February 2010
- "One million metric tons of CO2 stored underground in Illinois - KurzweilAI". kurzweilai.net.