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Amulet
Quebec, Canada
Main commodities: Cu Zn Au Ag


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The Amulet group of Archaean (2.8 Ga) volcanic hosted massive sulphide deposit is located 13 km NW of Noranda in Quebec, Canada.

The deposits of the operation included:

  East Waite - 1.5 Mt @ 4.1 % Cu, 3.25 % Zn, 31 g/t Ag, 1.8 g/t Au
  Waite-Amulet - 1.129 Mt @ 4.7% Cu, 2.97% Zn, 23.8 g/t Ag, 1.2 g/t Au
  Amulet A - 0.19 Mt @ 2.37 % Cu, 6.12 % Zn, 46 g/t Ag, 2 g/t Au
  Amulet Lower A - 4.69 Mt @ 5.14 % Cu, 5.28 % Zn, 44 g/t Ag, 1.4 g/t Au
  Amulet Upper A - 0.19 Mt @ 2,37 % Cu, 6.12 % Zn, 46 g/t Ag, 2 g/t Au
  Amulet C - 0.544 Mt @ 2.2 % Cu, 8.5 % Zn, 95.6 g/t Ag, 0.65 g/t Au
  Amulet F - 0.254 Mt @ 3.54 % Cu, 3.4 % Zn, 5.1 g/t Ag, 0.58 g/t Au
  Amulet 11 - 0.45 Mt @ 3.65 % Cu, 2.38 % Zn, 29 g/t Ag, 0.7 g/t Au
  Corbet - 2.8 Mt @ 2.99 % Cu, 2.13 % Zn, 19 g/t Ag, 0.76 g/t Au
  Old Waite - 1.12 Mt @ 4.7 % Cu, 2.98 % Zn, 22 g/t Ag, 1.1 g/t Au
  Millenbach - 3.2 Mt @ 3.43 % Cu, 4.23 % Zn, 42.5 g/t Ag, 0.72 g/t Au
  Norbec - 3.7 Mt @ 2.78 % Cu, 4.76 % Zn, 31.9 g/t Ag, 0.5 g/t Au

These are polymetallic volcanogenic hosted massive sulphide deposits as pyrite-pyrrhotite-chalcopyrite-sphalerite ore that were deposited directly on the Archaean Waite Andesite, deposited within the Noranda Cauldron. The host volcanic succession is dominated by massive andesitic flows, dacitic flows, gabbro and dioritic intrusions that are probably subvolcanics. In many locations, the andesite are variably chloritised, sericitised and pyritic.

See the main Noranda record for more background.

For detail see the reference(s) listed below.

The most recent source geological information used to prepare this decription was dated: 2000.    
This description is a summary from published sources, the chief of which are listed below.
© Copyright Porter GeoConsultancy Pty Ltd.   Unauthorised copying, reproduction, storage or dissemination prohibited.


    Selected References
Beaty D W, Taylor H P  1982 - Some petrologic and oxygen isotopic relationships in the Amulet Mine, Noranda, Quebec and their bearing on the origin of Archean massive sulfide deposits: in    Econ. Geol.   v77 pp 95-108
Gibson H L, Watkinson D H, Comba C D  1983 - Silicification: hydrothermal alteration in an Archean geothermal system within the Amulet Ryolite Formation, Noranda, Quebec: in    Econ. Geol.   v78 pp 954-971
Kerr D J, Gibson H L  1993 - A comparison of the Horne volcanogenic massive Sulfide deposit and intracauldron deposits of the mine sequence, Noranda, Quebec: in    Econ. Geol.   v88 pp 1419-1442


Porter GeoConsultancy Pty Ltd (PorterGeo) provides access to this database at no charge.   It is largely based on scientific papers and reports in the public domain, and was current when the sources consulted were published.   While PorterGeo endeavour to ensure the information was accurate at the time of compilation and subsequent updating, PorterGeo, its employees and servants:   i). do not warrant, or make any representation regarding the use, or results of the use of the information contained herein as to its correctness, accuracy, currency, or otherwise; and   ii). expressly disclaim all liability or responsibility to any person using the information or conclusions contained herein.

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