Cite
Trace elemental and sulfur-lead isotopic variations in metamorphosed volcanogenic massive sulfide (VMS) mineralization systems: An example from the Keketale Pb-Zn(-Ag) deposit, NW China.
MLA
Yu, Peng-Peng, et al. “Trace Elemental and Sulfur-Lead Isotopic Variations in Metamorphosed Volcanogenic Massive Sulfide (VMS) Mineralization Systems: An Example from the Keketale Pb-Zn(-Ag) Deposit, NW China.” Ore Geology Reviews, vol. 125, Oct. 2020, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.oregeorev.2020.103685.
APA
Yu, P.-P., Zheng, Y., & Wang, C.-M. (2020). Trace elemental and sulfur-lead isotopic variations in metamorphosed volcanogenic massive sulfide (VMS) mineralization systems: An example from the Keketale Pb-Zn(-Ag) deposit, NW China. Ore Geology Reviews, 125, N.PAG. https://doi.org/10.1016/j.oregeorev.2020.103685
Chicago
Yu, Peng-Peng, Yi Zheng, and Cheng-Ming Wang. 2020. “Trace Elemental and Sulfur-Lead Isotopic Variations in Metamorphosed Volcanogenic Massive Sulfide (VMS) Mineralization Systems: An Example from the Keketale Pb-Zn(-Ag) Deposit, NW China.” Ore Geology Reviews 125 (October): N.PAG. doi:10.1016/j.oregeorev.2020.103685.