"Interpreting Diamond Morphology" - Part II
by Valentin Afanasiev, Nikolai Zinchuk,
Valeriy Sonin, Elena Semenets

Rough Diamond Review, September 2004


The last post-magmatic stage of the kimberlite process has a lesser influence on the morphology of diamonds when compared to the pre- and syn- magmatic growth stages. These influences principally affect the surface of the diamonds and in some cases cause partial cracking. Trigons can be transformed through hexagonal forms into inverted trigons, while a tetrahexahedroidal shape can be formed at the same time. In one of the pipes of the Alakinskyi diamond field (Yakutia), surface alterations took place under the influence of hydrothermal fluids, which resulted from a sill intersecting the pipe. The sill altered the diamond morphology to a high degree, in some cases completely destroying the diamonds in contact zones of the sill. . .

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