“…The E-W lineaments were developed during the break-up of Gondwana, and therefore have been active since the Triassic period, as have many of the NWtrending faults, whereas the NE-trending faults have apparently remained inactive (Zalán et al, 1987(Zalán et al, , 1990. Jacques et al (2010Jacques et al ( , 2012, studying the structural lineaments along the eastern margin of the Paraná Basin and its basement in Santa Catarina by means of digital products (LANDSAT and SRTM images on 1:100,000 and 1:500,000 scales), defined the directions as follows: N-S and NNE-SSW (basement), NW-SE and N-S (Gondwana I Supersequence) and NE-SW and NW-SE (Gondwana III Supersequence -Serra Geral Formation) and concluded that SRTM 1:100,000 has the best results for the extractions of brittle lineaments (Fig. 1C).…”