Cite
Geochemical characteristics of organic carbon and pyrite sulfur in Ordovician-Silurian transition shales in the Yangtze Platform, South China: Implications for the depositional environment.
MLA
Xi, Zhaodong, et al. “Geochemical Characteristics of Organic Carbon and Pyrite Sulfur in Ordovician-Silurian Transition Shales in the Yangtze Platform, South China: Implications for the Depositional Environment.” Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 563, Feb. 2021, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.palaeo.2020.110173.
APA
Xi, Z., Tang, S., Lash, G. G., Zhang, B., & Lin, D. (2021). Geochemical characteristics of organic carbon and pyrite sulfur in Ordovician-Silurian transition shales in the Yangtze Platform, South China: Implications for the depositional environment. Palaeogeography, Palaeoclimatology, Palaeoecology, 563, N.PAG. https://doi.org/10.1016/j.palaeo.2020.110173
Chicago
Xi, Zhaodong, Shuheng Tang, Gary G. Lash, Bing Zhang, and Donglin Lin. 2021. “Geochemical Characteristics of Organic Carbon and Pyrite Sulfur in Ordovician-Silurian Transition Shales in the Yangtze Platform, South China: Implications for the Depositional Environment.” Palaeogeography, Palaeoclimatology, Palaeoecology 563 (February): N.PAG. doi:10.1016/j.palaeo.2020.110173.