The Daldyno‑Alakitsky area is located in the basin of the upper reaches of the Markha and Alakita rivers, in the northeastern marginal part of the Tunguska syneclise. Certain issues of the geological structure of the area have been considered in a number of works. The authors of these works make contradictory conclusions about the distribution patterns of kimberlite bodies and the time of formation of fold and fault structures due to different opinions about the nature of the relationship between kimberlites and traps, the conditions and sequence of their manifestation...