Suitability of surficial media for Ni–Cu–PGE exploration in an established mining camp: a case study from the South Range of the Sudbury Igneous Complex, Canada

Author:

Hashmi Sarah1ORCID,Leybourne Matthew I.12ORCID,Hamilton Stewart3,Layton-Matthews Daniel1ORCID,McClenaghan M. Beth4

Affiliation:

1. Queen's Facility for Isotope Research, Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, Ontario, Canada K7L 3N6

2. Arthur B. McDonald Canadian Astroparticle Physics Research Institute, Department of Physics, Engineering Physics and Astronomy, Queen's University, Kingston, Ontario, Canada K7L 3N6

3. Ontario Geological Survey, 933 Ramsey Lake Road, Sudbury, Ontario, Canada P3E 6B5

4. Geological Survey of Canada, 601 Booth St., Ottawa, Ontario, Canada K1A 0E9

Abstract

A geochemical study over the southwestern part of the South Range of the Sudbury Igneous Complex was completed to assess the suitability of surficial media (humus, B-horizon soil and C-horizon soil) for delineating geochemical anomalies associated with Ni–Cu–PGE (platinum group element) mineralization. Another objective was to test whether Na pyrophosphate can eliminate the effects of anthropogenic contamination in humus. Results of this study suggest that the natural geochemical signature of humus is strongly overprinted by anthropogenic contamination. Despite no indication of underlying or nearby mineralization, metal concentrations in humus samples by aqua regia collected downwind from smelting operations are higher compared to background, including up to 13 times higher for Pt, 12 times higher for Cu and nine times higher for Ni. The high anthropogenic background masks the geogenic signal such that it is only apparent in humus samples collected in the vicinity of known Ni–Cu–PGE deposits. Results of this study also demonstrate that anthropogenically derived atmospheric fallout also influences the upper B-horizon soil; however, lower B-horizon soil (at >20 cm depth) and C-horizon soil (both developed in till) are not affected. Glacial dispersal from Ni–Cu–PGE mineralization is apparent in C-horizon till samples analysed in this study. Compared to the background concentrations, the unaffected C-horizon till samples collected immediately down-ice of the low-sulfide, high precious metal Vermilion Cu–Ni–PGE deposit are enriched over 20 times in Pt (203 ppb), Au (81 ppm) and Cu (963 ppm), and over 30 times in Ni (1283 ppm).Supplementary material: supplementary tables and figures are available at https://doi.org/10.6084/m9.figshare.c.5691080

Publisher

Geological Society of London

Subject

General Earth and Planetary Sciences,Geochemistry and Petrology,General Environmental Science,General Chemistry

Reference129 articles.

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2. Ames, D.E. and Farrow, C.E.G. 2007. Metallogeny of the Sudbury mining camp, Ontario. In: Goodfellow, W.D. (ed.) Mineral Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods. Geological Association of Canada, Mineral Deposits Division, Special Publication no. 5, 329–350.

3. Ames, D.E. , Davidson, A. , Buckle, J.L. and Card, K.D. 2005. Geology, Sudbury bedrock compilation, Ontario. Open File 4570.

4. Pb-Sr-Nd Isotopes in Surficial Materials at the Pebble Porphyry Cu-Au-Mo Deposit, Southwestern Alaska: Can the Mineralizing Fingerprint be Detected Through Cover?

5. Patterns of insect communities along a stress gradient following decommissioning of a Cu-Ni smelter;Babin-Fenske;Environmental Pollution,2011

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