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• W2006558336 abstract "Research Article| January 01, 1999 Liquefaction Evidence for at Least Two Strong Holocene Paleo-Earthquakes in Central and Southwestern Illinois, USA WILLIAM E. MCNULTY; WILLIAM E. MCNULTY U. S. Geological Survey, Reston, VA 20192 Search for other works by this author on: GSW Google Scholar STEPHEN F. OBERMEIER STEPHEN F. OBERMEIER U. S. Geological Survey, Reston, VA 20192 Search for other works by this author on: GSW Google Scholar Environmental and Engineering Geoscience (1999) V (2): 133–146. https://doi.org/10.2113/gseegeosci.V.2.133 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation WILLIAM E. MCNULTY, STEPHEN F. OBERMEIER; Liquefaction Evidence for at Least Two Strong Holocene Paleo-Earthquakes in Central and Southwestern Illinois, USA. Environmental and Engineering Geoscience 1999;; V (2): 133–146. doi: https://doi.org/10.2113/gseegeosci.V.2.133 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentBy SocietyEnvironmental and Engineering Geoscience Search Advanced Search Abstract Two strong mid-Holocene earthquakes in Illinois have been documented by paleoliquefaction features such as clastic dikes, sills, and detachments of fine-grained sediment that sunk into liquefied sand. At least one paleo-earthquake occurred in central Illinois about 35 km NE of Springfield, probably sometime between 5,900 and 7,400 yr BP. Dike widths are as much as 0.4 m near the energy center of the earthquake. Outward from this center, dike widths attenuate and ultimately disappear at about 35 km. More than one paleo-earthquake is probably represented by liquefaction features near Springfield. Another paleo-earthquake that appears to have been centered about 65 km ESE of St. Louis, Missouri, occurred near 5,700 yr BP. The energy center is inferred as being in Illinois, and most likely near lowermost Shoal Creek where the meizoseismal region is defined by dikes as wide as 0.5 m and by a regional abundance of dikes. Dikes from this earthquake probably extend at least as far as 35 km from its inferred energy center. The earthquake near Shoal Creek and one earthquake near Springfield almost certainly exceeded M 6. The paleomagnitudes can be more closely bracketed by geotechnical testing and analysis, when used in conjunction with existing data. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article." @default.
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• W2006558336 title "Liquefaction Evidence for at Least Two Strong Holocene Paleo-Earthquakes in Central and Southwestern Illinois, USA" @default.
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