Geological interpretation of a sedimentary basin

The work presented in this master thesis work aims to illustrate the processing steps done on the seismic data acquired in the area of Val Duron, Trentino Alto Adige, Italy. The output of the analysis is described and the adequate geological model is used for the geological interpretation of this seismic data. The geological model will be also used to explain the dipping phenomenon of the Dolomite formations under the volcanic formations. The comparison with other geophysical techniques, like GPR, EM, and Audio- Magnetotellurics are carried out, to refine the geological interpretation and to prove the reliability and the accuracy of the seismic acquisitions in the meanwhile.