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西藏邦铺钼铜多金属矿床位于西藏冈底斯斑岩铜矿带东段,是典型的大型斑岩型矿床,以钼、铜为主,共生铅、锌。矿区内出露的地层除第四系(Q4)外,主要为古近系典中组(E1d)火山岩和下二叠统洛巴堆组(P1l)灰岩(大理岩)。前人研究表明,二长花岗斑岩为成矿母岩,古近系典中组(E1d)火山岩则为(含矿)围岩。前人虽然对该矿床做了大量的研究工作,但主要针对该矿床
The Bangpu molybdenum-copper polymetallic deposit in Tibet is located in the eastern part of the Gangdese porphyry copper belt in Tibet. It is a typical large-scale porphyry deposit dominated by molybdenum and copper and symbiotic lead and zinc. The strata exposed in the mining area are mainly Quaternary (E1d) volcanic rocks of the Paleogene and Lobolith group (P1l) limestone (marble) of the Lower Permian except Quaternary (Q4). Previous studies show that the granodiorite porphyry is the metallogenic parent rock, and the Paleogene Palaeo-Clarity (E1d) volcanic rock is (ore-bearing) rock. Although predecessors did a lot of research on the deposit, but mainly for the deposit