Abstract
In the late decades, the GPR was established as a high resolution method used in shallow investigations of the sub-surface, in many different applications. In the area, the Cuiabá Group is composed by a sequence of folded layers of phyllites and metasandstones, whose structures and arrangement could be well defined in the GPR profiles, including some quartz veins. In these lithotypes, the best reflectors correspond to the interfaces of the sandy layers, due the high electrical resistivity of the quartz in comparison to clay minerals.
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