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TitleRelevance of a Lithogeochemical Database To Epidemiological Studies in Central Saskatchewan, Canada
AuthorDunn, C E; Irvine, D G
SourceEnvironmental Geochemistry, Selected Papers From the 2nd International Symposium, Uppsala, Sweden, 16 - 19 September 1991; by Hitchon, B (ed.); Fuge, R (ed.); Applied Geochemistry no. 2, 1993 p. 215-222,
Alt SeriesGeological Survey of Canada, Contribution Series 36491
PublisherElsevier BV
MeetingSecond International Symposium On Environmental Geochemistry; Uppsala; Se; September 16-19, 1991
Mediapaper; on-line; digital
File formatpdf
NTS73A; 73B; 73C/SE; 73C/NE; 73F/SE; 73F/NE; 73G; 73H
AreaMeadow Lake; Saskatoon; Prince Albert; Henribourg
Lat/Long WENS-109.0000 -102.0000 54.0000 52.0000
Subjectssurficial geology/geomorphology; geochemistry; mathematical and computational geology; engineering geology; wells; lithogeochemistry; shales; sedimentary rocks; calcium geochemistry; cadmium geochemistry; molybdenum geochemistry; selenium geochemistry; uranium geochemistry; vanadium geochemistry; arsenic geochemistry; copper geochemistry; nickel geochemistry; antimony geochemistry; strontium geochemistry; zinc geochemistry; data collections; groundwater geochemistry; hydrologic environment; statistical analysis; statistical methods; analyses; trace element analyses; geochemical analyses; drillholes; glacial history; glaciation; glaciers; glacial deposits; Great Falls Tectonic Zone; Bearpaw Formation; Judith River Formation; Lea Park Formation; White Speckled Shales; White Specks Formation; Big River Formation; Viking Formation; Joli Fou Formation; Colorado Group; Mannville Group; Cretaceous
Illustrationsanalyses; sketch maps
Released1993 01 01
AbstractArchived drill-cuttings of Cretaceous sedimentary rocks from 96 wells were analyzed to provide a geochemical database and maps of a 100,000 km2 area of bedrock in central Saskatchewan. A dark shale (the White Speckled Shale) is enriched in Ca, Cd, Mo, Se, U and V (and to a lesser degree in As, Cu, Ni, Sb, Sr and Zn), when compared to other geological strata in the district. This shale subcrops beneath glacial drift near Henribourg, where there is a coincidence of structural weakness and formation water discharge. Because groundwater chemistry is controlled mostly by rock and sediment chemistry, the possibility was examined that the enrichment of some elements in the White Speckled Shale may have a bearing on the high incidence of childhood homes of Multiple Sclerosis patients at Henribourg. The lithogeochemical study provides basic data that may be of use in epidemiological studies.

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