Cite
Paleolake salinity evolution in the Qaidam Basin (NE Tibetan Plateau) between ~42 and 29 Ma: Links to global cooling and Paratethys sea incursions.
MLA
Ye, Chengcheng, et al. “Paleolake Salinity Evolution in the Qaidam Basin (NE Tibetan Plateau) between ~42 and 29 Ma: Links to Global Cooling and Paratethys Sea Incursions.” Sedimentary Geology, vol. 409, Nov. 2020, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.sedgeo.2020.105778.
APA
Ye, C., Yang, Y., Fang, X., Zhang, W., Song, C., & Yang, R. (2020). Paleolake salinity evolution in the Qaidam Basin (NE Tibetan Plateau) between ~42 and 29 Ma: Links to global cooling and Paratethys sea incursions. Sedimentary Geology, 409, N.PAG. https://doi.org/10.1016/j.sedgeo.2020.105778
Chicago
Ye, Chengcheng, Yibo Yang, Xiaomin Fang, Weilin Zhang, Chunhui Song, and Rongsheng Yang. 2020. “Paleolake Salinity Evolution in the Qaidam Basin (NE Tibetan Plateau) between ~42 and 29 Ma: Links to Global Cooling and Paratethys Sea Incursions.” Sedimentary Geology 409 (November): N.PAG. doi:10.1016/j.sedgeo.2020.105778.