Cite
Oxygen isotopic alteration rate of continental crust recorded by detrital zircon and its implication for deep-time weathering.
MLA
Li, Gaojun, et al. “Oxygen Isotopic Alteration Rate of Continental Crust Recorded by Detrital Zircon and Its Implication for Deep-Time Weathering.” Earth & Planetary Science Letters, vol. 578, Jan. 2022, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.epsl.2021.117292.
APA
Li, G., Yang, R., Xu, Z., Hartmann, J., Hedding, D. W., Li, X., Ernst, R. E., Li, Z.-H., Zou, H., Li, Z., & Chen, J. (2022). Oxygen isotopic alteration rate of continental crust recorded by detrital zircon and its implication for deep-time weathering. Earth & Planetary Science Letters, 578, N.PAG. https://doi.org/10.1016/j.epsl.2021.117292
Chicago
Li, Gaojun, Ruiyu Yang, Zhewen Xu, Jens Hartmann, David W. Hedding, Xianhua Li, Richard E. Ernst, et al. 2022. “Oxygen Isotopic Alteration Rate of Continental Crust Recorded by Detrital Zircon and Its Implication for Deep-Time Weathering.” Earth & Planetary Science Letters 578 (January): N.PAG. doi:10.1016/j.epsl.2021.117292.