Cite
Ca. 815 Ma intra-plate granitoids and mafic dykes from Emeishan pluton in the western Yangtze Block, SW China: A record of rifting during the breakup of Rodinia.
MLA
Zou, Hao, et al. “Ca. 815 Ma Intra-Plate Granitoids and Mafic Dykes from Emeishan Pluton in the Western Yangtze Block, SW China: A Record of Rifting during the Breakup of Rodinia.” Precambrian Research, vol. 371, Apr. 2022, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.precamres.2022.106569.
APA
Zou, H., Li, Y., Huang, C.-C., Said, N., Jiang, X.-W., Liu, H., Li, M., Chen, H.-F., Liu, C.-M., & Lan, Z.-W. (2022). Ca. 815 Ma intra-plate granitoids and mafic dykes from Emeishan pluton in the western Yangtze Block, SW China: A record of rifting during the breakup of Rodinia. Precambrian Research, 371, N.PAG. https://doi.org/10.1016/j.precamres.2022.106569
Chicago
Zou, Hao, Yang Li, Chang-Cheng Huang, Nuru Said, Xiu-Wei Jiang, Hang Liu, Min Li, Hai-Feng Chen, Chun-Mei Liu, and Zhong-Wu Lan. 2022. “Ca. 815 Ma Intra-Plate Granitoids and Mafic Dykes from Emeishan Pluton in the Western Yangtze Block, SW China: A Record of Rifting during the Breakup of Rodinia.” Precambrian Research 371 (April): N.PAG. doi:10.1016/j.precamres.2022.106569.