FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2164752147> ?p ?o ?g. }

• W2164752147 endingPage "1495" @default.
• W2164752147 startingPage "1475" @default.
• W2164752147 abstract "Research Article| October 01, 2000 Glacial and nonglacial sediment contributions to Wisconsin Episode loess in the central United States David A. Grimley David A. Grimley 1Illinois State Geological Survey, 615 East Peabody Drive, Champaign, Illinois 61820, USA Search for other works by this author on: GSW Google Scholar Author and Article Information David A. Grimley 1Illinois State Geological Survey, 615 East Peabody Drive, Champaign, Illinois 61820, USA Publisher: Geological Society of America Received: 08 Feb 1999 Revision Received: 07 Sep 1999 Accepted: 22 Nov 1999 First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2000) 112 (10): 1475–1495. https://doi.org/10.1130/0016-7606(2000)112<1475:GANSCT>2.0.CO;2 Article history Received: 08 Feb 1999 Revision Received: 07 Sep 1999 Accepted: 22 Nov 1999 First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation David A. Grimley; Glacial and nonglacial sediment contributions to Wisconsin Episode loess in the central United States. GSA Bulletin 2000;; 112 (10): 1475–1495. doi: https://doi.org/10.1130/0016-7606(2000)112<1475:GANSCT>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 The relative contributions of various glacial and nonglacial sediments to Wisconsin Episode loess units along the lower Illinois and central Mississippi Valleys are estimated on the basis of a comparison of magnetic susceptibility and silt and clay mineralogy. A mathematical method of source area calculation, using four compositional parameters, was guided by current knowledge of the regional glacial history. On the basis of this technique, the Roxana Silt, along the Illinois and Mississippi River Valleys, is composed of significant Superior lobe sediment (35%–40%) as well as Wadena or Des Moines lobe sediment (about 35%). This can account for its high magnetic susceptibility, feldspar content, kaolinite content, and pink hue. Lower Peoria Silt contains about 25%–35% Lake Michigan lobe sediment with reduced contributions of the other sources. After the Mississippi River's diversion (20.4 ka), the supply of Superior, Des Moines, and Wadena lobe sediment was cut off from the Illinois Valley in favor of Lake Michigan lobe sediment (75%–80% contribution). This major source area shift accounts for higher dolomite and illite contents and a more yellow hue in approximately the upper two-thirds of Peoria Silt in the study area. In loess south of St. Louis, less pronounced compositional shifts occur because Superior lobe sediment was not cut off and because Des Moines lobe, Wadena lobe, and Missouri River sediments, having more intermediate composition, compose 40%–50% of the loess, thereby diluting other source area changes. Nonglacial sediment, from fluvial and periglacial sources, is estimated to compose 10%–40% of loess in both regions. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2164752147 created "2016-06-24" @default.
• W2164752147 creator A5035435236 @default.
• W2164752147 date "2000-10-01" @default.
• W2164752147 modified "2023-09-27" @default.
• W2164752147 title "Glacial and nonglacial sediment contributions to Wisconsin Episode loess in the central United States" @default.
• W2164752147 cites W1191133777 @default.
• W2164752147 cites W1499431037 @default.
• W2164752147 cites W1573062526 @default.
• W2164752147 cites W1610356470 @default.
• W2164752147 cites W162173771 @default.
• W2164752147 cites W1665684728 @default.
• W2164752147 cites W1964325013 @default.
• W2164752147 cites W1966170689 @default.
• W2164752147 cites W1968647951 @default.
• W2164752147 cites W1970078895 @default.
• W2164752147 cites W1982875647 @default.
• W2164752147 cites W1997253102 @default.
• W2164752147 cites W2006932176 @default.
• W2164752147 cites W2009443939 @default.
• W2164752147 cites W2017941009 @default.
• W2164752147 cites W2026930890 @default.
• W2164752147 cites W2030315729 @default.
• W2164752147 cites W2033927353 @default.
• W2164752147 cites W2037998247 @default.
• W2164752147 cites W2038602359 @default.
• W2164752147 cites W2040152247 @default.
• W2164752147 cites W2045433471 @default.
• W2164752147 cites W2049830390 @default.
• W2164752147 cites W2054015957 @default.
• W2164752147 cites W2073205734 @default.
• W2164752147 cites W2076937137 @default.
• W2164752147 cites W2092471264 @default.
• W2164752147 cites W2097427881 @default.
• W2164752147 cites W2101390450 @default.
• W2164752147 cites W2101874561 @default.
• W2164752147 cites W2106743652 @default.
• W2164752147 cites W2122557672 @default.
• W2164752147 cites W2136182680 @default.
• W2164752147 cites W2138304154 @default.
• W2164752147 cites W2167658349 @default.
• W2164752147 cites W2290539442 @default.
• W2164752147 cites W2411753372 @default.
• W2164752147 cites W2416148648 @default.
• W2164752147 cites W2525467488 @default.
• W2164752147 cites W2588490037 @default.
• W2164752147 cites W2590540734 @default.
• W2164752147 cites W2591889804 @default.
• W2164752147 cites W2592619199 @default.
• W2164752147 cites W2594511499 @default.
• W2164752147 cites W2762460131 @default.
• W2164752147 doi "https://doi.org/10.1130/0016-7606(2000)112<1475:gansct>2.0.co;2" @default.
• W2164752147 hasPublicationYear "2000" @default.
• W2164752147 type Work @default.
• W2164752147 sameAs 2164752147 @default.
• W2164752147 citedByCount "58" @default.
• W2164752147 countsByYear W21647521472012 @default.
• W2164752147 countsByYear W21647521472013 @default.
• W2164752147 countsByYear W21647521472014 @default.
• W2164752147 countsByYear W21647521472015 @default.
• W2164752147 countsByYear W21647521472017 @default.
• W2164752147 countsByYear W21647521472018 @default.
• W2164752147 countsByYear W21647521472019 @default.
• W2164752147 countsByYear W21647521472020 @default.
• W2164752147 countsByYear W21647521472021 @default.
• W2164752147 countsByYear W21647521472022 @default.
• W2164752147 crossrefType "journal-article" @default.
• W2164752147 hasAuthorship W2164752147A5035435236 @default.
• W2164752147 hasConcept C11413529 @default.
• W2164752147 hasConcept C127313418 @default.
• W2164752147 hasConcept C136764020 @default.
• W2164752147 hasConcept C151730666 @default.
• W2164752147 hasConcept C15739521 @default.
• W2164752147 hasConcept C161191863 @default.
• W2164752147 hasConcept C166957645 @default.
• W2164752147 hasConcept C199360897 @default.
• W2164752147 hasConcept C2778447006 @default.
• W2164752147 hasConcept C2778805511 @default.
• W2164752147 hasConcept C2780154274 @default.
• W2164752147 hasConcept C2781113848 @default.
• W2164752147 hasConcept C41008148 @default.
• W2164752147 hasConcept C48103436 @default.
• W2164752147 hasConcept C95457728 @default.
• W2164752147 hasConceptScore W2164752147C11413529 @default.
• W2164752147 hasConceptScore W2164752147C127313418 @default.
• W2164752147 hasConceptScore W2164752147C136764020 @default.
• W2164752147 hasConceptScore W2164752147C151730666 @default.
• W2164752147 hasConceptScore W2164752147C15739521 @default.
• W2164752147 hasConceptScore W2164752147C161191863 @default.
• W2164752147 hasConceptScore W2164752147C166957645 @default.
• W2164752147 hasConceptScore W2164752147C199360897 @default.
• W2164752147 hasConceptScore W2164752147C2778447006 @default.
• W2164752147 hasConceptScore W2164752147C2778805511 @default.
• W2164752147 hasConceptScore W2164752147C2780154274 @default.
• W2164752147 hasConceptScore W2164752147C2781113848 @default.
• W2164752147 hasConceptScore W2164752147C41008148 @default.
• W2164752147 hasConceptScore W2164752147C48103436 @default.
• W2164752147 hasConceptScore W2164752147C95457728 @default.

• next