Twenty-five zircon megacrysts were recovered from a large sample (approximately 100 L of gravel, screened to -2.0 mm in the field; Berryman et al. 1999) collected downslope from the TC-01 kimberlite, which occurs as a small pipe-like outcrop. The zircon grains are characterised by an almost complete absence of crystal faces. They are typically rounded to subrounded, and display a large range of
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