U-Pb Detrital Zircon Ages and Geochemical Features of the Jingxing Formation, (Qamdo Basin, Tibet: Implications): Inferences for the Metallogenic Model of the East Tethys Evaporite.

MLA

Han, Wenhua, et al. “U-Pb Detrital Zircon Ages and Geochemical Features of the Jingxing Formation, (Qamdo Basin, Tibet: Implications): Inferences for the Metallogenic Model of the East Tethys Evaporite.” Minerals (2075-163X), vol. 11, no. 7, July 2021, p. 745. EBSCOhost, https://doi.org/10.3390/min11070745.

APA

Han, W., Ma, H., Fang, W., Cheng, H., Li, Y., Li, B., Miao, W., & Hai, Q. (2021). U-Pb Detrital Zircon Ages and Geochemical Features of the Jingxing Formation, (Qamdo Basin, Tibet: Implications): Inferences for the Metallogenic Model of the East Tethys Evaporite. Minerals (2075-163X), 11(7), 745. https://doi.org/10.3390/min11070745

Chicago

Han, Wenhua, Haizhou Ma, Weixuan Fang, Huaide Cheng, Yongshou Li, Binkai Li, Weiliang Miao, and Qinyu Hai. 2021. “U-Pb Detrital Zircon Ages and Geochemical Features of the Jingxing Formation, (Qamdo Basin, Tibet: Implications): Inferences for the Metallogenic Model of the East Tethys Evaporite.” Minerals (2075-163X) 11 (7): 745. doi:10.3390/min11070745.