Abstract
The Golden Giant mine is developed in the Archean Hemlo gold-molybdenum deposit hosted within the Hemlo-Heron Bay greenstone belt in NW Ontario, Canada. The ore occurs in steeply dipping tabular zones within metasedimentary rocks and within quartz-eye muscovite schists in association with microcline-mica-pyrite alteration, and a variety of other minerals. It is proposed that the primary Au-Mo mineralization occurred before the M1 metamorphic event, possibly related to emplacement of the Golden Giant quartz porphyry in a premineralization structural zone. The mineralization was modified by the M1 event, and severely deformed during mylonitization. Dikes from the Cedar Creek stock intruded the deposit sequence and overprinted the M1 event with an M2 metamorphism. -from Authors
Original language | English (US) |
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Pages (from-to) | 720-756 |
Number of pages | 37 |
Journal | Economic Geology |
Volume | 89 |
Issue number | 4 |
DOIs | |
State | Published - 1994 |