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| | Mineral Deposits of Canada - Regional Metallogeny Ni-Cu-PGE: Metallogeny of the Sudbury Mining Camp, Ontario |
 | | The Sudbury Igneous Complex (SIC) is a Paleoproterozoic (1850 ± 1 Ma) hypabyssal intrusion consisting of a lower, ore-bearing sublayer, noritic to gabbro cumulates overlain by granophyre produced during impact by melting of the lower crust and carbonaceous sediments (Krogh et al., 1984; Grieve,1994; Mungall et al., 2004). |
 | | Sudbury ore deposits are divided into 3 main types (Coats and Snyder, 1984; Morrison et al., 1994) based on their interrelated environments: Contact deposits, Offset and Footwall deposits all containing Ni-Cu-PGE however, the latter have elevated and locally very high PGE contents (Fig. |
 | | Totten) and/or Sudbury breccia in the vicinity of the dyke (ie. |
| gsc.nrcan.gc.ca /mindep/metallogeny/ni_cu_pge/sudbury/index_e.php (8726 words) |
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