Carbonate reservoir diagenesis associated to connate water/fresh water interaction within a thermal aquifer located in the central-northern part of the Moesian Platform (Romania)

Abstract

The Moesian Platform sedimentary basin, which occupies large parts of Romania and of Bulgaria, includes a several hundred meters thick carbonate formation of Late Jurassic – Early Cretaceous age. The regional aquifer hosted by that reservoir formation has been tapped by several deep (up to 3,300 m) wells, drilled in southern Romania during the late 1980s and early 1990

Keywords

• sedimentary basin
• connate water
• freshwater
• diagenesis
• calcite retrograde solubility
• moesian platform