*Senior Lecturer, Almalyk branch of Tashkent State Technical University, Uzbekistan
**Senior Teacher, Almalyk branch of Tashkent State Technical University, Uzbekistan
Online published on 12 February, 2021.
The Sary-Chekku copper deposit is considered to have a complex tectonic structure. The deposit is composed mainly of sedimentary and effusive rocks. As the quarry deepens, there is a systematic decrease in the level of groundwater. The article provides information and conclusions on the distribution of areas depending on the hydrogeological conditions of the field, the lithological composition of interfering rocks, circulation and accumulation, types of groundwater in terms of distribution depth and form of occurrence, direction of movement of groundwater trash, total and seasonal discharge.
Fault, Hydrogeological Conditions, Water Inflow, Groundwater Levels, Hydrogeological Conditions, Aquifer, Groundwater, Fracturing, Groundwater, Fractured Groundwater, Fractured Vein Water, Water Cut
