HYDRODYNAMIC OVERACTIVITY FLUIDS IN FRACTURES - INDICATOR OF TECTONIC FAULTS

Abstract

Existence of orthogonal coaxial and regmatic grid of fractures, revealed in the thickness of Astrakhan arch is proven by hydrodynamic overactivity fluids in fractures, which compose the Bashkirian layers in its limits.

Keywords

• астраханский свод
• разломы
• трещины
• керн
• пористость
• проницаемость