By I Prigogine
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Extra info for Advances in Chemical Physics, Vol.2 (Interscience 1958)
Eds) 2009. Application of till and stream sediment heavy mineral and geochemical methods to mineral exploration in western and northern Canada; Geological Association of Canada Short Course Notes 18. H. 1911. Prospecting in Nova Scotia. Nova Scotia Mining Society Journal, 16, 7391. W. 1971. Till studies and their application to regional drift prospecting. Canadian Mining Journal, 92, 45-50. W. 1975. Principles of geochemical exploration for sulphide deposits using shallow samples of glacial drift.
MCCURDY. W. B. 2007. Cretaceous shale of northern Alberta: A new frontier for base metal exploration. In: MILKEREIT, B. ) Exploration in the New Millennium, Proceedings of the Fifth Decennial International Conference on Mineral Exploration, 1207-1213. C. R. 2006. Indicator mineral content and geochemistry of glacial sediments from northwest Alberta (NTS 84L, M): new opportunities for mineral exploration. Geological Survey of Canada, Open File 5121 and Alberta Geological Survey, Special Report 77.
The GSLSZ, projected to surface (Eaton & Hope 2003), is shown as the thick dashed line. Large arrows depict ice flow during glacial maximum and smaller arrows indicate local lobes of flow during deglaciation. Fig. 4. Histogram of δ34S values for sphalerite grains from NW Alberta till samples, the Pine Point Pb-Zn deposit and other Pb-Zn deposits in the Rocky and Mackenzie mountains (Paradis et al. 2006). 0 per mil (Evans et al. 1968). 2006). Modelling of U and Pb concentrations and ratios suggest a depleted lower crustal source consistent with Pb derivation from basement rocks (Nelson et al.