Mathematical modeling of thermomechanical erosion beneath Proterozoic komatiitic basaltic sinuous rilles in the Cape Smith Belt, New Québec, Canada
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Authors
Williams, D
Kerr, Ross
Lesher, C.M.
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Springer
Abstract
Virtually all of the economic Ni-Cu-(platinum group element (PGE)) mineralization in the central part of the Cape Smith Belt of New Québec is hosted by thick olivine cumulate units in the Katinniq Member of the Raglan Formation at the base of the 1. 9 Ga
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Mineralium Deposita
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Restricted until
2037-12-31