Ultra-fresh, complexly zoned olivines from the Benfontein kimberlite.
Two distinct xenocrystic core populations from the base of the SCLM.
Type 1 cores represent metasomatic alteration by early kimberlite melts.
Multiple growth stages from ultramafic to mafic kimberlite compositions.
Late-stage evolution to carbonatitic compositions in the crust.
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