Cite
Magnesium isotopic composition of back-arc basin lavas and its implication for the recycling of serpentinite-derived fluids.
MLA
Ding, Yi, et al. “Magnesium Isotopic Composition of Back-Arc Basin Lavas and Its Implication for the Recycling of Serpentinite-Derived Fluids.” Marine Geology, vol. 453, Nov. 2022, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.margeo.2022.106921.
APA
Ding, Y., Jin, X., Li, X., Li, Z., Liu, J., Wang, H., Zhu, J., Zhu, Z., & Chu, F. (2022). Magnesium isotopic composition of back-arc basin lavas and its implication for the recycling of serpentinite-derived fluids. Marine Geology, 453, N.PAG. https://doi.org/10.1016/j.margeo.2022.106921
Chicago
Ding, Yi, Xianglong Jin, Xiaohu Li, Zhenggang Li, Jiqiang Liu, Hao Wang, Jihao Zhu, Zhimin Zhu, and Fengyou Chu. 2022. “Magnesium Isotopic Composition of Back-Arc Basin Lavas and Its Implication for the Recycling of Serpentinite-Derived Fluids.” Marine Geology 453 (November): N.PAG. doi:10.1016/j.margeo.2022.106921.