Carbonate rock hypergenesis

Hypergenesis transforms rock families differently. Surface carst forms occur in limestone and dolomite in the altitude range from highland to depression in all climatic zones, and underground forms – caves and shafts, calmatation bodies and carst waters are formed there as well. Contact hypergenesis is a specific type of destruction. Covered carst is presented by a system of sedimentation reservoirs with deposits transformed up to allites and bauxites.