Publication Type:Journal Article
Source:Economic Geology and the Bulletin of the Society of Economic GeologistsEconomic Geology and the Bulletin of the Society of Economic Geologists, Economic Geology Publishing Company, Lancaster, PA, United States, Volume 109, Number 2, p.367-386 (2014)
Keywords:amphibolite facies, Canada, copper ores, deformation, disseminated deposits, eastern canada, fabric, facies, faults, fractional crystallization, geochemistry, grade, greenschist facies, magmas, melts, metal ores, metals, Metamorphic rocks, metamorphism, mineral deposits, genesis, mineralization, nickel ores, Ontario, ore bodies, ore-forming fluids, partial melting, partition coefficients, platinum group, platinum ores, sampling, solid solution, Sudbury District Ontario, Sudbury structure, textures, thrust faults
The Garson Ni-Cu-platinum group element (PGE) deposit is a deformed, overturned, contact-type deposit along the contact between the Sudbury Igneous Complex and underlying rocks of the Huronian Supergroup in the South Range of the 1850 Ma Sudbury structure. The main Garson orebodies occur along steeply S dipping ductile shear zones, which formed as D (sub 1) north-over-south amphibolite facies thrust zones that were rotated and overturned during buckling of the Sudbury Igneous Complex. The shear zones were reactivated as south-over-north greenschist facies reverse shear zones during D (sub 2) . The mineralization is primarily composed of pyrrhotite-pentlandite-chalcopyrite-magnetite, occurring as four main types: (1) disseminated to matrix-textured sulfides in Main Mass norite and slivers of norite within shear zones, (2) semimassive breccia ore within the shear zones, (3) quartz-calcite-sulfide veins spatially associated with breccia ores, and (4) Cu-Pd-Pt-Au-rich "footwall-type" mineralization in the nearby Garson Ramp deposit. Garson disseminated sulfides and breccia ores have relatively low Pd/Ir ratios and restricted ranges of Ni tenors and Fe/Ni ratios, very similar to those of undeformed disseminated sulfides and contact-type massive ores at the less deformed Creighton deposit. This suggests that the mobilization of the breccia ores by ductile plastic flow during D (sub 1) and D (sub 2) did not significantly alter their original magmatic geochemical signatures. Garson breccia ores are slightly depleted in Cu-Pt-Pd-Au and slightly enriched in Rh-Ru-Ir relative to disseminated sulfides, similar to other contact-type deposits at Sudbury. In contrast, quartz-calcite-sulfide veins at Garson are characterized by very low Rh-Ru-Ir abundances and very high Pd/Ir ratios, consistent with their mobilization and deposition from metamorphic-hydrothermal fluids. Despite being strongly enriched in Cu-Pd-Pt-Au, there are too few of these veins to account for the broad depletion in Cu-Pd-Pt-Au from the main mass of breccia ores, suggesting that the breccia ores are monosulfide solid solution cumulates that left a residual sulfide melt represented by the Cu-Pd-Pt-Au-rich ores in the Garson Ramp deposit.
GeoRef, Copyright 2018, American Geological Institute.<br/>2014-004500<br/>Garson Mine