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We report the mineralogy and high precision microprobe trace element data of olivine from the Mesoproterozoic, diamondiferous P3 kimberlite in the Wajrakarur Kimberlite Field (WKF), southern India. Olivine macrocrysts in the kimberlite exhibit a core–rim structure which offers an opportunity to examine the variation in their minor and trace element (Ni, Ca, Al, Ti, Mn, Cr and Na) contents in order to differentiate melt-derived olivines from mantle olivines and also to distinguish multiple populations of mantle olivines.

The P3 kimberlite, Wajrakarur kimberlite field, India: mineralogy, and major and trace element compositions of olivines as records of their magmatic versus xenocrystic origin