Detecting faults and stratigraphy in limestone with Ground-Penetrating Radar: A case study in Rustrel

Surface Ground-Penetrating Radar (GPR) data have been acquired along the floor as well as along the vertical walls of a tunnel inside a karstic limestone reservoir in Rustrel. Geological study previously demonstrated the existence of stratification planes with an average dip of 25° to the south and numerous subvertical fault planes. The mono-offset GPR profile analysis acquired along the vertical wall of the tunnel demonstrates the presence of dipping reflectors that can be followed as deep as 16 m from the acquisition surface with 250 MHz nominal antennas. The position of these reflectors coincides with observations of faults recorded in a report written during the tunnel excavations.