Distribuzione dei carbonati metano-derivati e fluidi freddi nella successione plio-pleistocenica nell'area del fiume Secchia

The objectiveof this thesis is to identify the cause of the accretion of carbonate concretions along the banks of the river Secchia. First, it proved essential to consult documentation both to understand the origin and characteristics of these concretions, and to have an idea of how the whole area presents itself and its history, since on-site investigations were impossible. Detailed geological sections of the area were then drawn up and their study attempted to identify the cause of the carbonate growth mentioned above.