Barnes Sarah-Jane, Coutur J.F., Sawyer Edward W. et Bouchaib C.. (1993). Nickel-copper occurrences in the Belleterre-Angliers Belt of the Pontiac Subprovince and the use of Cu-Pd ratios in interpreting platinum-group element distributions. Economic Geology, 88, (6), p. 1402-1418.
URL officielle: http://econgeol.geoscienceworld.org/content/88/6/1...
Within the Belleterre-Angliers greenstone belt of the Pontiac subprovince there are a number of Ni-Cu sulfide occurrences associated with synvolcanic gabbros. The stratigraphy and geochemistry of the belt suggest that it is a rifted island arc and that the gabbros which contain the Ni-Cu sulfides were derived from the mantle plume that rifted the island arc.The conditions under which the sulfides formed may be modeled either by recalculating the sulfide compositions to 100 percent sulfide or by using the Cu/Pd ratios. Both approaches suggest that most of the sulfide occurrences formed from an enriched MORB magma with R factors of 200 to 1,000. One of the occurrences (La Force) is depleted in platinum-group elements (PGE) relative to Cu and this depletion may be the result of the removal of sulfides from the magma prior to emplacement at this stratigraphic level.The advantage of using the Cu/Pd ratio rather than recalculating to 100 percent sulfide is that it is not necessary to have S analyses to model the conditions of formation of the sulfides. Further, the Cu/Pd ratio may be used as a prospecting tool. Rocks with ratios greater than mantle values formed from magmas depleted in Pd, possibly due to removal of sulfide from the magma. This implies the potential for a PGE-bearing sulfide deposit at stratigraphically lower levels. Such an approach has been applied to PGE targets in the eastern Abitibi subprovince. Samples from four Ni-Cu occurrences with Cu/Pd ratios close to mantle ratios have the potential to produce PGE as a by-product. Samples from seven Ni-Cu sulfide occurrences and the layered intrusions Lac Dore, Bell River, and Cummings Complex have Cu/Pd ratios much greater than mantle ratios, indicating that these intrusions and sulfides are not good targets for PGE at this stratigraphic level, although there may be PGE-rich sulfides present at depth.
|Type de document:||Article publié dans une revue avec comité d'évaluation|
|Version évaluée par les pairs:||Oui|
|Sujets:||Sciences naturelles et génie > Sciences naturelles > Sciences de la terre (géologie, géographie)|
|Département, module, service et unité de recherche:||Départements et modules > Département des sciences appliquées > Unité d'enseignement en sciences de la Terre|
|Mots-clés:||Abitibi Belt, Baby Group, basalts, Belleterre-Angliers Belt, Canada, Canadian Shield, chemical composition, copper, copper ores, Cummings Complex, distribution, Eastern Canada, équations, felsic composition, gabbros, geochemistry, greenstone belts, igneous rocks, intrusions, island arcs, Lac des Bois Group, layered intrusions, lithophile elements, mafic composition, magmas, mantle, mantle plumes, metal ores, metals, metamorphic belts, mid-ocean ridge basalts, mineral exploration, nickel ores, North America, ore grade, palladium, platinum group, plutonic rocks, Pontiac Subprovince, Québec, stratigraphy, sulfides, Superior Province, volcanic rocks, volcaniclastics|
|Déposé le:||14 juin 2016 17:19|
|Dernière modification:||09 déc. 2016 15:37|
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