CARBONATITIC MELT INCLUSIONS WITH CO2 AND CH4 IN HEALED CRACKS IN A DIAMOND
Since the diamond is type IIa with pronounced dislocation network patterns (visible in cathodoluminescence imaging), we tentatively link this sample to the sublithospheric diamond variety known as CLIPPIR diamonds. The carbonatitic melt inclusions could have been trapped later at shallower depths, but since the dislocation networks conform to the healed cracks, the melt may have been trapped in sublithospheric mantle before the final stages of dislocation network formation. At the very least, the melt being sealed into healed cracks attests to it being trapped at diamond-stable depths in the mantle. The fact that the inclusions are trapped in cracks suggests the melt was associated with potentially violent stresses, overstepping the typical plastic high-temperature deformation behavior of diamond, perhaps associated with ascent of the diamond and/or early stages of kimberlite volcanism. Melt inclusions of similar carbonatitic composition have previously been documented in healed cracks in mantle-derived olivine xenocrysts from the Koala kimberlite (Ekati mine, Canada). These melt inclusions may be valuable, direct evidence of the nature of carbonatitic melts at mantle depths.