Tabiiy fanlar

STUDY OF GEOLOGICAL-STRUCTURAL, LITHOLOGICAL-FACIES CONDITIONS OF THE DISTRIBUTION OF FRESH GROUNDWATER WITHIN THE ADYR AND PRIADYR ZONES

Geological-structural, lithological-facies factors, pebble lenses, tectonic disturbances, deep faults, weakened zones

Authors

  • Музаффар ЖУРАЕВ Доктор философии (Ph.D) по геологии, старший научный сотрудник Университета Геологических Наук при Госкомгеологии РУз,, Uzbekistan
  • Абумуслим ЗУЛФУКОРОВ Докторант Институт гидрогеологии и инженерной геологии при Университете Геологических Наук. Узбекистан, Uzbekistan

Based on the generalization of data from all previously conducted geological and geophysical works, the prospects of
groundwater in the Chust-Papskaya, Kasansai and Namangan Adyr zones were analyzed and evaluated. As a result, specific
natural features were identified (transverse and longitudinal tectonic disturbances, weakened zones, the roof of Neogene deposits,
the direction of groundwater flow, the feeding area, areas of groundwater accumulation). During the formation of fresh
groundwater in the Neogene column, Paleogene waters participate, i.e. the discharge of groundwater goes through the crushing
zones.