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Zeng QD, QinKZ, Liu JM, Li GM, Zhai MG, Chu SX,Guo YP. 2015.Porphyry molybdenum deposits in the Tianshan-Xingmeng orogenic belt, northern China. International Journal of Earth Sciences,104(4): 991-1023; Su BX, Qin KZ, Lu YH, Sun H., Sakyi PA. 2015. Decoupling of whole-rock Nd-Hf and zircon Hf-O isotopic compositions of a 284 Ma mafic-ultramafic
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Zeng QD, QinKZ, Liu JM, Li GM, Zhai MG, Chu SX,Guo YP. 2015.Porphyry molybdenum deposits in the Tianshan-Xingmeng orogenic belt, northern China. International Journal of Earth Sciences,104(4): 991-1023; Su BX, Qin KZ, Lu YH, Sun H., Sakyi PA. 2015. Decoupling of whole-rock Nd-Hf and zircon Hf-O isotopic compositions of a 284 Ma mafic-ultramafic
WhatsAppGet PriceGet A QuoteThe epithermal 1954, Santo Tomas II, Philippines, in 1958, Panguna, Papua orebodies associated with the Far Southeast deposit, Philip- New Guinea, in 1972, and Grasberg, Indonesia in 1989. pines (Claveria et al., 1999), and the carbonate-hosted poly- Gold-only end members were first discovered in the Mari-metallic orebodies alongside the Bingham deposit (Babcock cunga belt of northern Chile in
WhatsAppGet PriceGet A QuoteThe Maricunga belt is a linear metallogenic unit defined by at least 14 zones of gold and/or silver mineralization between latitudes 26 degrees and 28 degrees S in the Andean Cordillera of northern Chile. After 10 years of exploration, three precious metal deposits are in production, two more have proven reserves, and others are being drilled. Total geologic reserves are 420 metric tons of
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WhatsAppGet PriceGet A QuoteThe epithermal 1954, Santo Tomas II, Philippines, in 1958, Panguna, Papua orebodies associated with the Far Southeast deposit, Philip- New Guinea, in 1972, and Grasberg, Indonesia in 1989. pines (Claveria et al., 1999), and the carbonate-hosted poly- Gold-only end members were first discovered in the Mari-metallic orebodies alongside the Bingham deposit (Babcock cunga belt of northern Chile in
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WhatsAppGet PriceGet A QuoteThese data support our contention that this green- stone belt initially formed as a northern Philippines-like ac- cretionary complex (Lucas et al., 1995). 2. GEOLOGICAL SETTING The Paleoproterozoic Tram-Hudson Orogen is cored by the ein- deer Zone(Fig. 1 ), a 400 km-wide amalgam of greenstone belts and intervening sedimentary and plutonic domains that has been in- terpreted as a broad
WhatsAppGet PriceGet A QuoteThe Atlas porphyry Cu–Au deposit is located in central Cebu Island in the Philippines, with a proven mineral reserve of 1420 Mt at 0.45% Cu, 0.24 g/t Au, 0.018 g/t Mo, and 1.8 g/t Ag. It is associated with the Lutopan quartz diorite porphyry stock that was emplaced into the Cretaceous volcano-sedimentary sequences of the Cansi Formation. Two stages of hypogene alteration have been identified
WhatsAppGet PriceGet A QuoteAges from the "Mogod Formation" of the Permian-Triassic igneous rocks in the Sayan-Baikal belt, Northern Mongolia. Nagoya Univ. Museum No. Khishigsuren Sodnom, Manchuk Nuramkhaan, Ser-Od Tseden-Ish, Bayarmaa Batsaikhan, 2019.
WhatsAppGet PriceGet A QuoteThe epithermal 1954, Santo Tomas II, Philippines, in 1958, Panguna, Papua orebodies associated with the Far Southeast deposit, Philip- New Guinea, in 1972, and Grasberg, Indonesia in 1989. pines (Claveria et al., 1999), and the carbonate-hosted poly- Gold-only end members were first discovered in the Mari-metallic orebodies alongside the Bingham deposit (Babcock cunga belt of northern Chile in
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