Browse

In the East Carpathians Bend region (Romania), a salt formation was deposited during the lowermost Miocene (Aquitanian-Burdigalian). Subsequently, the salt reached present-day structural positions by diapiric piercing of the overlying sedimentary deposits. As a result, a multitude of isolated ? although quite large - outcrops of salt diapirs are encountered nowadays. In this complex geological setting, a great number of salt karst phenomena occur, generating dolines, sinkholes and salt caves. The surface topograph...