Sample of chlorite-altered mafic intrusion at south end of Central Zone with crystalline molybdenite remobilized onto fracture planes; up to 350 ppm molybdenum in grab sample. This presence of molybdenite is rare in a mafic intrusion setting and was one of the first clues towards an intrusion-related copper-gold deposit model as source for high-grade mineralization further north along the CZ structure.
Sample of chlorite-altered mafic intrusion at south end of Central Zone with crystalline molybdenite remobilized onto fracture planes; up to 350 ppm molybdenum in grab sample. This presence of molybdenite is rare in a mafic intrusion setting and was one of the first clues towards an intrusion-related copper-gold deposit model as source for high-grade mineralization further north along the CZ structure.