fracture-controlled quartz-reef enclosed in a pink granitoid body surrounded by grey-
granitoids constituting the regional matrix. Sulfide-bearing stringers, pegmatites with only
quartz+ microcline and sulfide disseminations, all within the pink-granitoid, represent other
minor modes of occurrences. Despite this diversity in mode of occurrence, the mineralogy of
ores is quite consistent and conform to a common paragenetic sequence comprising an …