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• W2912255001 abstract "The Taipingzhen deposit is a newly discovered REE deposit in the North Qinling Orogen (NQO), Central China. The REE ores are hosted in the altered fracture zones of Paleozoic strata and a granitic intrusion. The ore minerals mainly include bastnäsite-(Ce)[(Ce(CO3)F], parisite-(Ce)[CaCe2(CO3)3F2], and synchysite-(Ce)[CaCe(CO3)2F], and this deposit also contains some uncommon minerals, such as törnebohmite-(Ce)[Ce2Al(SiO4)2(OH)], gatelite-(Ce) [CaCe3AlAl2Mg(Si2O7)(SiO4)3O(OH)2], fluocerite-(La)[LaF3] and F-rich cerite-(Ce)[(Ce,Ca)9 Mg(SiO4)3[SiO3(OH)]4F3], which are identified here for the first time in China. To determine the timing of REE mineralization and explore possible genetic relationships between mineralization and granitic magmatism, the U-Pb ages of bastnäsite-(Ce) from ore and zircon from ore-hosting granite are obtained. The in situ LA-MC-ICP-MS U-Pb age of the bastnäsite-(Ce) provides a reliable 238U/206Pb-207Pb/206Pb lower intersection point age of 409 ± 16 Ma, and ID-TIMS analyses yield an U-Pb age of 407.8 ± 3.3 Ma; the U-Pb dating of the magmatic zircon reveals that the wall rock was emplaced at 457.1 ± 4.9 Ma, and the hydrothermal zircon age of 399.4 ± 3.5 Ma records the time of hydrothermal alteration, thus indicating that the REE mineralization in the Taipingzhen deposit occurred at approximately 409–400 Ma. This age coincides well with the U-Pb ages of the bastnäsite-(Ce) and zircon, revealing a genetic association between the hydrothermal fluid and the REE mineralization. The Hf isotopic compositions imply that the partial melting of Paleoproterozoic HP and UHP eclogite from the lower crust provided ore materials for the mineralization, and the deposit was generated in a retrograde metamorphic setting during the late Paleozoic postcollisional extension event in the NQO. Furthermore, combined with the geochronological data published for other U-REE metallic deposits in the NQO, our study indicates that the late Silurian-early Devonian granite-related U-REE metallic mineralization throughout the NQO mainly occurred during 421–395 Ma." @default.
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• W2912255001 date "2019-04-01" @default.
• W2912255001 modified "2023-10-15" @default.
• W2912255001 title "In situ LA-MC-ICP-MS and ID-TIMS U-Pb ages of bastnäsite-(Ce) and zircon from the Taipingzhen hydrothermal REE deposit: New constraints on the later Paleozoic granite-related U-REE mineralization in the North Qinling Orogen, Central China" @default.
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• W2912255001 cites W1993407228 @default.
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• W2912255001 cites W2005633590 @default.
• W2912255001 cites W2007105153 @default.
• W2912255001 cites W2008693928 @default.
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• W2912255001 cites W2017220828 @default.
• W2912255001 cites W2022865240 @default.
• W2912255001 cites W2023685791 @default.
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• W2912255001 cites W2028200216 @default.
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• W2912255001 cites W2032391096 @default.
• W2912255001 cites W2034513010 @default.
• W2912255001 cites W2035422468 @default.
• W2912255001 cites W2037950492 @default.
• W2912255001 cites W2038907544 @default.
• W2912255001 cites W2047904277 @default.
• W2912255001 cites W2048272718 @default.
• W2912255001 cites W2061189874 @default.
• W2912255001 cites W2063754919 @default.
• W2912255001 cites W2068260939 @default.
• W2912255001 cites W2074325170 @default.
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• W2912255001 cites W2092386709 @default.
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• W2912255001 cites W2157256234 @default.
• W2912255001 cites W2226676496 @default.
• W2912255001 cites W2298989339 @default.
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• W2912255001 doi "https://doi.org/10.1016/j.jseaes.2019.02.002" @default.
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