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TitreThe Lemoine auriferous volcanogenic massive sulfide deposit, Chibougamau camp, Abitibi Greenstone Belt, Quebec, Canada: geology and genesis
AuteurMercier-Langevin, P; Lafrance, B; Bécu, V; Dubé, B; Kjarsgaard, I; Guha, J
SourceArchean volcanism, magmatism and ore deposits; par Mercier-Langevin, P (éd.); Hannington, M (éd.); Gibson, H (éd.); Houlé, M (éd.); Dubé, B (éd.); Monecke, T (éd.); Goutier, J (éd.); Economic geology and the bulletin of the Society of Economic Geologists vol. 109, no. 1, 2014 p. 231-269,
Séries alt.Secteur des sciences de la Terre, Contribution externe 20120014
ÉditeurSociety of Economic Geologists
Documentpublication en série
Mediapapier; en ligne; numérique
SNRC32G/09; 32G/10; 32G/15; 32G/16
Lat/Long OENS-75.0000 -74.0000 50.0000 49.5000
Sujetsgîtes volcanogènes; gîtes sulfureux; Archéen; métallogénie; altération; assemblages de minéraux; métamorphisme; faciès à schiste vert; déformation; chlorite; séricité; épidote; chloritoïde; cadre tectonique; or; minéralisation; altération hydrothermale; gisements minéraux hydrothermaux; lithologie; roches volcaniques; rhyolites; dacites; andésites; basaltes; gabbros; porphyres; analyses géochimiques; géochimie des éléments en trace; géochimie des éléments majeurs; Ceinture d'Abitibi Greenstone ; Formation de Waconichi ; minéraux métalliques; géologie structurale; pétrologie ignée et métamorphique; géochimie; Précambrien
Illustrationsgeological sketch maps; geochemical analyses
ProgrammeÉtude des gîtes de sulfures massifs volcaniques, Initiative géoscientifique ciblée (IGC-4)
ProgrammeÉtude des gîtes d'or, Initiative géoscientifique ciblée (IGC-4)
Diffusé2013 11 19
Résumé(disponible en anglais seulement)
The Lemoine auriferous volcanogenic massive sulfide deposit (0.76 Mt at 4.6 g/t Au, 4.2 wt % Cu, and 9.5 wt % Zn) is part of the Chibougamau camp located in the northeastern part of the Abitibi greenstone belt. The deposit is hosted by a steeply dipping, S-facing homoclinal volcanic succession (~2729-2726 Ma Waconichi Formation, Lemoine Member) composed of effusive and intrusive tholeiitic rhyolites and andesites cut by comagmatic diorite and gabbro dikes and overlain by transitional to mildly calc-alkaline basalts, andesites, and rhyolites.
Seven predominant synvolcanic alteration assemblages, now intensely deformed and metamorphosed to upper greenschist facies, were defined based on their mineralogy and position relative to ore. Albite-quartz, sericite-carbonate, sericite-chlorite, sericite-chlorite-(Zn), and chlorite-sericite-epidote-carbonate assemblages define semiconcordant zones that are stacked from the paleoseafloor to the deep footwall. In contrast, chlorite and chlorite-sericite-chloritoid assemblages overprint the other alteration zones and form subconcordant to now transposed discordant zones in the deposit footwall. Most alteration assemblages are characterized by relative SiO2, CaO, and Na2O mass losses and relative FeO, MgO, K2O, and CO2 mass gains. Whole-rock oxygen isotopes indicate that the temperatures of alteration ranged from ~100° to 150°C (sericite-carbonate assemblage) to >=350°C (sericite-chlorite, chlorite-sericite-chloritoid, and chlorite assemblages). The chlorite-sericite-chloritoid assemblage, and to some extent the sericite-chlorite assemblage, are associated with strong to near total depletion of light rare earth elements possibly due to reaction with Cl-bearing, mildly acidic fluids at depth in the ore-forming hydrothermal system.
The sulfide lens was formed in part on the seafloor and in part by subseafloor replacement. The massive sulfides are particularly rich in Bi, suggesting a possible magmatic input into the Lemoine ore-forming hydrothermal system. High Bi concentrations in the mineralizing system are likely to have enhanced Au precipitation by scavenging the precious metal from the hydrothermal fluids. The Au-rich nature of the Lemoine auriferous volcanogenic massive sulfide deposit can be explained by a combination of very efficient metal transport, highly effective capture of metals at or near the seafloor, and a possible magmatic contribution to the hydrothermal system.