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- W2393971878 abstract "The newly discovered Tuolugou deposit in Qinghai Province, northwestern China is the first independent, large SEDEX cobalt (gold) deposit and the cobalt orebodies are hosted by quartz albitite. Rhenium and osmium isotopes in pyrite from different types of ores in the deposit have been used to determine the timing of mineralization by ICP-MS. Pyrite samples have very low rhenium and osmium concentrations varying in the range 0.122～8.988 ng/g and 0.00313～0.05366 ng/g, respectively, however, isotope data of seven pyrite samples yield an isochron age of 432±23 Ma (2σ) on the 187 Re / 188 Os versus 187 Os / 188 Os plot and an age of 442±17 Ma (2σ) on the 187 Re versus 187 Os correlation diagram, which suggests that the age of the widespread Naij Tal Group is of early Paleozoic. Our result provides a new proof for plate splitting and mineralization taking place at the late Ordovician period in the eastern Kunlun orogenic belt, and is important for understanding the ore-forming processes and discussing tectonic evolution in the region." @default.
- W2393971878 created "2016-06-24" @default.
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- W2393971878 date "2006-01-01" @default.
- W2393971878 modified "2023-09-23" @default.
- W2393971878 title "Re-Os Isotopic Dating of Pyrite in the Tuolugou SEDEX Cobalt (Gold) Deposit, Golmud, Qinghai Province" @default.
- W2393971878 hasPublicationYear "2006" @default.
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