Heinonen, J. S., Fusswinkel, T., & Geography, D. o. G. a. (2017). High Ni and low Mn/Fe in olivine phenocrysts of the Karoo meimechites do not reflect pyroxenitic mantle sources. Chemical Geology, 467, 134.
Chicago Style (17th ed.) CitationHeinonen, Jussi S., Tobias Fusswinkel, and Department of Geosciences and Geography. "High Ni and Low Mn/Fe in Olivine Phenocrysts of the Karoo Meimechites Do Not Reflect Pyroxenitic Mantle Sources." Chemical Geology 467 (2017): 134.
MLA (9th ed.) CitationHeinonen, Jussi S., et al. "High Ni and Low Mn/Fe in Olivine Phenocrysts of the Karoo Meimechites Do Not Reflect Pyroxenitic Mantle Sources." Chemical Geology, vol. 467, 2017, p. 134.
Warning: These citations may not always be 100% accurate.