Chemical and isotopic indicators of groundwater evolution in the basal sands of a buried bedrock valley in the Midwestern United States; implications for recharge, rock-water interactions, and mixing

Buried bedrock valley aquifers can be found throughout Canada and the northern United States where glacial deposits have filled in previously exposed bedrock valleys. The Mahomet bedrock valley is an east-west-trending buried valley in central Illinois containing basal Pleistocene sands and gravels... Description complète

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doi: 10.1130/B26574.1
Auteurs:Hackley, K.C.; Panno, S.V.; Anderson, T.F.
Volume Volume Titre:Geological Society of America Bulletin
Source:Geological Society of America Bulletin, 122(7-8), p.1047-1066. Publisher: Geological Society of America (GSA), Boulder, CO, United States. ISSN: 0016-7606
Date de publication:2010
Remarque:In English. With GSA Data Repository Item 2009286. 92 refs.; illus., incl. sects., geol. sketch map
Sujets:Aquifers; Bedrock; Buried valleys; C-14; Carbon; Cenozoic; Clastic sediments; D/H; Deuterium; Experimental studies; Geochemistry; Ground water; Hydrochemistry; Hydrogen; Isotope ratios; Isotopes; Mixing; O-18/O-16; Oxygen; Paleohydrology; Pleistocene; Quaternary; Radioactive isotopes; Recharge; S-34/S-32; Sand; Sediments; Shallow aquifers; Stable isotopes; Sulfur; Tritium; Water-rock interaction; Illinois; Midwest; United States; Central Illinois; Mahomet Aquifer; Sankoty Mahomet Aquifer
Coordonnées:N400000 N410000 W0873000 W0900000
Identificateur:2010050185
Informations sur le Copyright:GeoRef, Copyright 2020 American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States, Reference includes data supplied by the Geological Society of America
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