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- W2108682664 abstract "Research Article| August 01, 2001 Origin of illite in the lower Paleozoic of the Illinois basin: Evidence for brine migrations Georg H. Grathoff; Georg H. Grathoff 1Department of Geology, Portland State University, Portland, Oregon 97207-0751, USA Search for other works by this author on: GSW Google Scholar Duane M. Moore; Duane M. Moore 2Illinois State Geological Survey, 615 East Peabody Drive, Champaign, Illinois 61820, USA Search for other works by this author on: GSW Google Scholar Richard L. Hay; Richard L. Hay 3Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar Klaus Wemmer Klaus Wemmer 4Institut für Geologie und Dynamik der Lithosphäre, Goldschmidtstrasse 3, Universität Göttingen, D-37077 Göttingen, Germany Search for other works by this author on: GSW Google Scholar Author and Article Information Georg H. Grathoff 1Department of Geology, Portland State University, Portland, Oregon 97207-0751, USA Duane M. Moore 2Illinois State Geological Survey, 615 East Peabody Drive, Champaign, Illinois 61820, USA Richard L. Hay 3Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Klaus Wemmer 4Institut für Geologie und Dynamik der Lithosphäre, Goldschmidtstrasse 3, Universität Göttingen, D-37077 Göttingen, Germany Publisher: Geological Society of America Received: 25 Aug 1999 Revision Received: 08 Aug 2000 Accepted: 27 Nov 2000 First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2001) 113 (8): 1092–1104. https://doi.org/10.1130/0016-7606(2001)113<1092:OOIITL>2.0.CO;2 Article history Received: 25 Aug 1999 Revision Received: 08 Aug 2000 Accepted: 27 Nov 2000 First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Georg H. Grathoff, Duane M. Moore, Richard L. Hay, Klaus Wemmer; Origin of illite in the lower Paleozoic of the Illinois basin: Evidence for brine migrations. GSA Bulletin 2001;; 113 (8): 1092–1104. doi: https://doi.org/10.1130/0016-7606(2001)113<1092:OOIITL>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract In the lower Paleozoic of the Illinois Basin, three illite polytypes are found: 2M1 of detrital origin, and 1Md and 1M of diagenetic origin. Illite polytype quantification of detrital 2M1 illite and diagenetic 1Md and 1M illite, combined with K-Ar age dating, allows extrapolation to apparent detrital and diagenetic illite ages. Kinetic modeling of smectite illitization, combined with the calculated age of illitization, can evaluate different origins of illite. The diagenetic illite in the lower Paleozoic of the Illinois Basin is interpreted not to have formed solely by burial diagenesis but mainly during multiple brine events.The Upper Ordovician Maquoketa Group contains diagenetic illite (dominantly 1Md with minor 1M) with an extrapolated age of ∼360 m.y. (356–377 m.y.) and formed from smectite at temperatures of 50–100 °C. This age falls within the span of dates for illite/smectite (I/S) in K-bentonites from the Upper Mississippi Valley and is interpreted to be a combined result of illitization by burial diagenesis and either a hydrothermal brine from the southern and deeper part of the basin or a K-rich brine from the Michigan Basin, Upper Mississippi Valley area, or Forest City Basin.In Ordovician and Cambrian shale partings and sandstone older than the Maquoketa Group, the diagenetic illite (1Md in shale and 1M in sandstone) has an age of ∼300 m.y. and formed at temperatures <140 °C. This late Paleozoic age falls within the range of illites from sandstone in the Upper Mississippi Valley and K-bentonites of the Appalachian Basin; it coincides with the Alleghany orogeny and is interpreted as having formed by gravity-driven flow from the uplifted Alleghanian-Ouachita orogenic belt that drove hot (<140 °C) fluids through the Illinois Basin. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2108682664 title "Origin of illite in the lower Paleozoic of the Illinois basin: Evidence for brine migrations" @default.
- W2108682664 cites W1487826653 @default.
- W2108682664 cites W1490199883 @default.
- W2108682664 cites W1501169336 @default.
- W2108682664 cites W1565933435 @default.
- W2108682664 cites W1591751245 @default.
- W2108682664 cites W1938525451 @default.
- W2108682664 cites W1952956830 @default.
- W2108682664 cites W1968649250 @default.
- W2108682664 cites W1970225661 @default.
- W2108682664 cites W1974608328 @default.
- W2108682664 cites W1991608935 @default.
- W2108682664 cites W1992692715 @default.
- W2108682664 cites W1993547842 @default.
- W2108682664 cites W2009740241 @default.
- W2108682664 cites W2023614917 @default.
- W2108682664 cites W2025178867 @default.
- W2108682664 cites W2029604943 @default.
- W2108682664 cites W2031811664 @default.
- W2108682664 cites W2032265832 @default.
- W2108682664 cites W2033993178 @default.
- W2108682664 cites W2049743598 @default.
- W2108682664 cites W2052694638 @default.
- W2108682664 cites W2055214313 @default.
- W2108682664 cites W2058618159 @default.
- W2108682664 cites W2073815295 @default.
- W2108682664 cites W2075579439 @default.
- W2108682664 cites W2075618665 @default.
- W2108682664 cites W2082767266 @default.
- W2108682664 cites W2084808637 @default.
- W2108682664 cites W2085255986 @default.
- W2108682664 cites W2089982870 @default.
- W2108682664 cites W2098803626 @default.
- W2108682664 cites W2101874561 @default.
- W2108682664 cites W2104922272 @default.
- W2108682664 cites W2118406625 @default.
- W2108682664 cites W2118743490 @default.
- W2108682664 cites W2119846469 @default.
- W2108682664 cites W2124082299 @default.
- W2108682664 cites W2138690333 @default.
- W2108682664 cites W2139307794 @default.
- W2108682664 cites W2141881543 @default.
- W2108682664 cites W2141959065 @default.
- W2108682664 cites W2152353204 @default.
- W2108682664 cites W2155405934 @default.
- W2108682664 cites W2157577438 @default.
- W2108682664 cites W2160568866 @default.
- W2108682664 cites W2162439861 @default.
- W2108682664 cites W2164646646 @default.
- W2108682664 cites W2164663173 @default.
- W2108682664 cites W2170787962 @default.
- W2108682664 cites W2198876721 @default.
- W2108682664 cites W2256864448 @default.
- W2108682664 cites W2314927865 @default.
- W2108682664 cites W2345486973 @default.
- W2108682664 cites W2480693151 @default.
- W2108682664 cites W2497917617 @default.
- W2108682664 cites W2593286661 @default.
- W2108682664 cites W2624079165 @default.
- W2108682664 cites W2749727196 @default.
- W2108682664 cites W2906133667 @default.
- W2108682664 cites W2921001871 @default.
- W2108682664 cites W3100563374 @default.
- W2108682664 cites W3124572718 @default.
- W2108682664 cites W3125571847 @default.
- W2108682664 cites W3127423911 @default.
- W2108682664 cites W324503581 @default.
- W2108682664 cites W602796201 @default.
- W2108682664 cites W85414462 @default.
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