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Mineral exploration in large parts of Canada is difficult because the bedrock is hidden beneath thick layers of glacially derived sediments. One technique to overcome this, called drift prospecting, identifies high concentrations of economically significant minerals or elements in the glacial sediments and helps to identify their bedrock sources. This project was designed to interpret Quaternary geology to assist in mineral development. This report shows how the geochemistry and lithology of the glacial sediments vary across the region and how the stratigraphy and provenance of those sediments can be interpreted so that geochemical anomalies or mineralized boulders may be traced back to their bedrock sources.
Integrated geological, geochemical and geophysical data for the posttectonic granitic rocks of the North Pole, Burnthill, Dungarvon, Trout Brook, and Rocky Brook plutons and surrounding areas were examined to assess their potential for uranium mineralization. Geological, geochemical, and geophysical criteria that are thought to be useful guides for uranium exploration were also established for the host granites.
Item is a compilation of research papers on the topic of geology in Canada in 1992. Each paper has its own abstract and bibliography.