Cite
Mesoproterozoic (∼1.3 Ga) S–type granites in Shangdu area, Inner Mongolia of the North China Craton (NCC): Implications for breakup of the NCC from the Columbia supercontinent.
MLA
Li, Changhai, et al. “Mesoproterozoic (∼1.3 Ga) S–type Granites in Shangdu Area, Inner Mongolia of the North China Craton (NCC): Implications for Breakup of the NCC from the Columbia Supercontinent.” Precambrian Research, vol. 369, Feb. 2022, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.precamres.2021.106515.
APA
Li, C., Liu, Z., Xu, Z., Dong, X., Liu, J., Cheng, Y., & Zhang, N. (2022). Mesoproterozoic (∼1.3 Ga) S–type granites in Shangdu area, Inner Mongolia of the North China Craton (NCC): Implications for breakup of the NCC from the Columbia supercontinent. Precambrian Research, 369, N.PAG. https://doi.org/10.1016/j.precamres.2021.106515
Chicago
Li, Changhai, Zhenghong Liu, Zhongyuan Xu, Xiaojie Dong, Jin Liu, Yusong Cheng, and Nuo Zhang. 2022. “Mesoproterozoic (∼1.3 Ga) S–type Granites in Shangdu Area, Inner Mongolia of the North China Craton (NCC): Implications for Breakup of the NCC from the Columbia Supercontinent.” Precambrian Research 369 (February): N.PAG. doi:10.1016/j.precamres.2021.106515.