FEATURES OF THE FORMATION OF NATURAL BRINES WITHIN THE QUARRY FIELD OF THE BOTUOBINSKAYA PIPE

The article briefly presents the geological and hydrogeological aspects of the Botuobinskaya kimberlite pipe located at the Nakyn production site. The chemical and filtration characteristics of water from the host sediments are analyzed the features of the geological structure and distribution of groundwater in the region are identified. As a result of the study, hypotheses are put forward regarding the origin of the detected brines and technical solutions have been proposed for efficient development of the deposit, considering hard hydrogeological conditions. These conclusions are important for a deeper understanding of geological processes and optimization of diamond production in this region.