SIGNS OF THE PRESENCE AND PROSPECTS FOR IDENTIFICATION OF HIGH DIAMOND-BEARING KIMBERLITES OF MIDDLE PALEOZOIC AGE IN THE TERRITORY OF THE OLENEK UPWAY AND ITS FRAMEWORK

The main perspectives of the primary sources of diamonds today are associated with the northeast of the Siberian Platform. Here there are reliable indications of Middle Paleozoic diamondiferous kimberlite bodies. These kimberlites are localized in the Anabar River basin, as well as in the area of the Kyutyungda graben and to the south in the upper reaches of the Daldyn and Molodo rivers, and in the Toluop-Daldyn watershed, including its northern slope.