Cite
Subducted carbonates not required: Deep mantle melting explains stable Ca isotopes in kimberlite magmas.
MLA
Antonelli, Michael A., et al. “Subducted Carbonates Not Required: Deep Mantle Melting Explains Stable Ca Isotopes in Kimberlite Magmas.” Geochimica et Cosmochimica Acta, vol. 348, May 2023, pp. 410–27. EBSCOhost, https://doi.org/10.1016/j.gca.2023.03.025.
APA
Antonelli, M. A., Giuliani, A., Wang, Z., Wang, M., Zhou, L., Feng, L., Li, M., Zhang, Z., Liu, F., & Drysdale, R. N. (2023). Subducted carbonates not required: Deep mantle melting explains stable Ca isotopes in kimberlite magmas. Geochimica et Cosmochimica Acta, 348, 410–427. https://doi.org/10.1016/j.gca.2023.03.025
Chicago
Antonelli, Michael A., Andrea Giuliani, Zaicong Wang, Meiling Wang, Lian Zhou, Lanping Feng, Ming Li, Zhaofeng Zhang, Fang Liu, and Russell N. Drysdale. 2023. “Subducted Carbonates Not Required: Deep Mantle Melting Explains Stable Ca Isotopes in Kimberlite Magmas.” Geochimica et Cosmochimica Acta 348 (May): 410–27. doi:10.1016/j.gca.2023.03.025.