GEOSCAN Search Results: Fastlink


TitleGlacial geology and glacial sediment geochemistry in the Clyde Forks - Westport area of Ontario
AuthorKettles, I M
SourceGeological Survey of Canada, Paper no. 91-17, 1992, 39 pages,
MapsPublication contains 4 maps
Map Info.surficial geology, lithological, 1:50,000
Mediapaper; on-line; digital
RelatedThis publication contains the following publications
RelatedThis publication is related to Spirito, W A; McClenaghan, M B; Plouffe, A; McMartin, I; Campbell, J E; Paulen, R C; Garrett, R G; Hall, G E M; (2011). Till sampling and analytical protocols for GEM Projects: from field to archive, Geological Survey of Canada, Open File 6850
File formatpdf
NTS31C/09; 31C/10; 31C/15; 31C/16; 31F/02; 31F/01
AreaClyde Forks; French Line; Carleton Palce; Lanark; Mcdonalds Corners; Elphin; Sharbot Lake; Tichborne; Westport; Perth; Smiths Falls; Ompah
Lat/Long WENS-77.0000 -76.0000 45.2500 44.5000
Subjectsgeochemistry; surficial geology/geomorphology; bedrock geology; tills; glaciofluvial deposits; glaciolacustrine deposits; organic deposits; alluvial deposits; ice movement; glacial history; wisconsinian glacial stage; glacial stages; glacial deposits; arsenic geochemistry; uranium geochemistry; manganese geochemistry; zinc geochemistry; cobalt geochemistry; eskers; drumlins; landforms; nickel geochemistry; iron geochemistry; copper geochemistry; chromium geochemistry; mercury geochemistry; silver geochemistry; gold geochemistry; molybdenum geochemistry; lead geochemistry; cadmium geochemistry; ice movement directions; drift deposits; invertebrates; fossils; pebble lithology; silts; drift geochemistry; sedimentary facies; facies; mineral occurrences; depositional environment; Robertson Lake Mylonite Zone; Ostracoda; Candona Subtriangulata; Mysis Relicta; Quaternary
Illustrationssketch maps; photographs
ProgramCanada-Ontario Mineral Development Agreement, 1985-1990
LinksCanadian Database of Geochemical Surveys, downloadable files
LinksBanque de données de levés géochimiques du Canada, fichiers téléchargeables
Released1992 11 01; 2013 05 29
AbstractAll glacial deposits in the Clyde Forks-Westport area are thought to be Late Wisconsinan or younger. The dominant direction of glacial flow during the Late Wisconsinan was south-southwestward. The most widespread surficial deposit is sandy, stony till. Glaciofluvial sands and gravels are widely distributed, and include deposits associated with three prominent esker-subaqueous fan systems. Laminated glaciolacustrine fine sand and silty clay occur in low-lying areas west of Perth and southeast of Westport. Similar silty clay deposits in the vicinity of Perth and Smiths Falls may be marine. Regional variations in carbonate content of glacial sediments and till texture reflect most strongly the effects of glacial transport. Concentrations of Paleozoic limestone clasts (2 .0-5.6 mm) and clay-sized detritus in till are high overlying Paleozoic terrane in the eastern part of the study region and over an area of Precambrian terrane which extends over 20 km west and southwest of the Paleozoic-Precambrian boundary. Much of the Precambrian terrane is underlain by carbonate-poor lithologies. In contrast, the trace element content of the clay-sized fraction of drift reflects, in most areas, composition of the underlying or nearby bedrock. For example, concentrations of As, Au, Hg, Cu, Pb, and Fe, are high over a major structural zone - the Robertson Lake Mylonite Zone where many known showings of gold and sulphide minerals are known. Further drift prospecting is recommended in the vicinity of the Robertson Lake Mylonite Zone as its mineral potential is largely untested.