ИСТИНА

Precipitation of diamonds and associated minerals from the parental silicate-carbonate-carbon melts-solutions through their cooling and consolidation in the upper mantle reservoirs-chambers are bound to generate the maximum potential for diamond deposits. However the kimberlitic magmas transferring diamonds from mantle to crust are capable to dissolve them in shorter lifting period and prolonged solidification durability in the crust cumulative chambers (on the eve of formation of the explosive kimberlitic pipes).