| Citation: |
Zi-jie Wu, Long-wei Qiu, Hai-peng Wang, Mi-shan Zhong, Pei-long Cui, 2019. New zircon U–Pb ages of the Xinghuadukou Group, Xing’an block and its geological implications, China Geology, 2, 393-395. doi: 10.31035/cg2018111
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New zircon U–Pb ages of the Xinghuadukou Group, Xing’an block and its geological implications
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References
[1] Nelson DR. 2001. An assessment of the determination of depositional ages for precambrian clastic sedimentary rocks by U–Pb dating of detrital zircons. Sedimentary Geology, 141/142, 37–60. doi: 10.1016/S0037-0738(01)00067-7 [2] Zhao YD, Xu FM, Che JY, Wang KL., Li SC., Wu DT. 2017. Constraints from the zircon U-Pb dating on the formation age and composition of the Xinhuadukou Group in northeastern Da Hinggan Mountains. Geology in China, 44(3), 575–587 (in Chinese with English abstract). doi: 10.12029/gc20170313 [3] Zong KQ, Klemd R, Yuan Y, He ZY, Guo JL, Shi XL, Liu YS, Hu ZC, Zhang ZM. 2017. The assembly of Rodinia: The correlation of early Neoproterozoic (ca. 900 Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB). Precambrian Research, 290, 32–48. doi: 10.1016/j.precamres.2016.12.010 -
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Zi-jie Wu, Long-wei Qiu, Hai-peng Wang, Mi-shan Zhong, Pei-long Cui, 2019. New zircon U–Pb ages of the Xinghuadukou Group, Xing’an block and its geological implications, China Geology, 2, 393-395. doi: 10.31035/cg2018111
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Figure 1.
Generalized geologic map of the Naiman area (a); U–Pb concordia diagram and representative CL image for zircons from the Xinghuadukou Group in the Naiman area (b); age frequency histogram for zircons from the Xinghuadukou Group in the Naiman area (c).