Abstract
Abstract Study of an area in the southern Grenville of Quebec, by a stream sediment reconnaissance survey, outlined a previously unknown nickel-copper occurrence. Both reconnaissance and detail soil surveys were employed to define the sources of the stream sediment anomalies. A rock geochemical survey was carried out along with the detail soil survey. Some of the soil and rock geochemical anomalies were drilled and in all cases low-grade nickel-copper mineralization was encountered.
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