For reconstructing formation conditions, the internal and real structures o
f microdiamonds from the Udachnaya kimberlite pipe were studied by the meth
ods of X-ray and cathode-luminescent topographies and IR spectroscopy.
One of the main elements of the internal irregularity of most microcrystals
Is a linear or a step-like zoning along {111}. Structurally, most microdia
monds have several domains significantly differing in physical characterist
ics. It is established that the periphery of microdiamond crystal always ha
s more A-type defects than B1-type ones. Such specific features are most ob
vious in octahedral microcrystals. Rounded microcrystals may have disturbed
primary-growth features as a result of their longer stay in the deep mediu
m. It has been revealed that cubic microcrystals have subparallel filaments
(with a small disordering angle), which are a sign of a normal growth mech
anism. This mechanism is realized owing to the higher degree of oversaturat
ion in the crystallization medium as compared with the layer-by-layer growt
h mechanism. Some cuboids have central zones saturated with discrete microi
nclusions of water and carbonates, which indicates the presence of a water-
carbonate fluid at the initial stages of the formation of such crystals.
The obtained data suggest that the microdiamond formation passes through se
veral stages. The alteration trend for some physical characteristics may be
st sign of the re:gular evolution of the Udachnaya-pipe microdiamonds.