Mantle source of the 2.44-2.50-Ga mantle plume-related magmatism in the Fennoscandian Shield: evidence from Os, Nd, and Sr isotope compositions of the Monchepluton and Kemi intrusions.

MLA

Yang, Sheng-Hong, et al. “Mantle Source of the 2.44-2.50-Ga Mantle Plume-Related Magmatism in the Fennoscandian Shield: Evidence from Os, Nd, and Sr Isotope Compositions of the Monchepluton and Kemi Intrusions.” Mineralium Deposita, vol. 51, no. 8, Dec. 2016, pp. 1055–73. EBSCOhost, https://doi.org/10.1007/s00126-016-0673-9.

APA

Yang, S.-H., Hanski, E., Li, C., Maier, W., Huhma, H., Mokrushin, A., Latypov, R., Lahaye, Y., O’Brien, H., & Qu, W.-J. (2016). Mantle source of the 2.44-2.50-Ga mantle plume-related magmatism in the Fennoscandian Shield: evidence from Os, Nd, and Sr isotope compositions of the Monchepluton and Kemi intrusions. Mineralium Deposita, 51(8), 1055–1073. https://doi.org/10.1007/s00126-016-0673-9

Chicago

Yang, Sheng-Hong, Eero Hanski, Chao Li, Wolfgang Maier, Hannu Huhma, Artem Mokrushin, Rais Latypov, Yann Lahaye, Hugh O’Brien, and Wen-Jun Qu. 2016. “Mantle Source of the 2.44-2.50-Ga Mantle Plume-Related Magmatism in the Fennoscandian Shield: Evidence from Os, Nd, and Sr Isotope Compositions of the Monchepluton and Kemi Intrusions.” Mineralium Deposita 51 (8): 1055–73. doi:10.1007/s00126-016-0673-9.