Geology and hydrothermal evolution of the Baituyingzi porphyry Mo (Cu) deposit, eastern Inner Mongolia, NE China: Implications for Mo and Cu precipitation mechanisms in CO2-rich fluids.

MLA

Sun, Yan, et al. “Geology and Hydrothermal Evolution of the Baituyingzi Porphyry Mo (Cu) Deposit, Eastern Inner Mongolia, NE China: Implications for Mo and Cu Precipitation Mechanisms in CO2-Rich Fluids.” Ore Geology Reviews, vol. 81, Mar. 2017, pp. 689–705. EBSCOhost, https://doi.org/10.1016/j.oregeorev.2016.03.023.

APA

Sun, Y., Liu, J., Zeng, Q., Wang, J., Wang, Y., Hu, R., Zhou, L., Wu, G., Gao, Y., & Shen, W. (2017). Geology and hydrothermal evolution of the Baituyingzi porphyry Mo (Cu) deposit, eastern Inner Mongolia, NE China: Implications for Mo and Cu precipitation mechanisms in CO2-rich fluids. Ore Geology Reviews, 81, 689–705. https://doi.org/10.1016/j.oregeorev.2016.03.023

Chicago

Sun, Yan, Jianming Liu, Qingdong Zeng, Jingbin Wang, Yuwang Wang, Ruizhong Hu, Lingli Zhou, Guanbin Wu, Yuyou Gao, and Wenjun Shen. 2017. “Geology and Hydrothermal Evolution of the Baituyingzi Porphyry Mo (Cu) Deposit, Eastern Inner Mongolia, NE China: Implications for Mo and Cu Precipitation Mechanisms in CO2-Rich Fluids.” Ore Geology Reviews 81 (March): 689–705. doi:10.1016/j.oregeorev.2016.03.023.