| Citation: |
Hua-lei Zhao, Jian-guo Li, Zhi-bin Xiao, Pei-sen Miao, Qing-hong Si, Lu-lu Chen, Reng-an Yu, Yin Chen, 2021. Determination of formation age (0.14 Ma) of the Pengyang sandstone-type uranium deposit in the Ordos Basin, China: Using pitchblende in situ femtosecond LA-MC-ICP-MS method, China Geology, 4, 747-748. doi: 10.31035/cg2021008
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Determination of formation age (0.14 Ma) of the Pengyang sandstone-type uranium deposit in the Ordos Basin, China: Using pitchblende in situ femtosecond LA-MC-ICP-MS method
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References
Cheng YH, Wang SY, Jin RS, Li JG, Ao C, Teng XM. 2019. Global Miocene tectonics and regional sandstone-style uranium mineralization. Ore Geology Review, 106, 238–250. doi: 10.1016/j.oregeorev.2019.02.003. Fayek M, Kyser TK, Riciputi LR. 2002. U and Pb isotope analysis of uranium minerals by ion microprobe and the geochronology of the McArthur River and Sue Zone uranium deposits, Saskatchewan, Canada. The Canadian Mineralogist, 40(6), 1553–1570. doi: 10.2113/gscanmin.40.6.1553. -
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Hua-lei Zhao, Jian-guo Li, Zhi-bin Xiao, Pei-sen Miao, Qing-hong Si, Lu-lu Chen, Reng-an Yu, Yin Chen, 2021. Determination of formation age (0.14 Ma) of the Pengyang sandstone-type uranium deposit in the Ordos Basin, China: Using pitchblende in situ femtosecond LA-MC-ICP-MS method, China Geology, 4, 747-748. doi: 10.31035/cg2021008
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Figure 1.
In situ femtosecond LA-MC-ICP MS pitchblende dating points noted on the backscattering photograph. Pit-pitchblende; Ab‒albite; Ant‒anatase; Qtz‒quartz; Cal‒calcite.
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Figure 2.
Pitchblende U-Pb isotopic concordant diagram for the Pengyang uranium deposit.