This work aim to obtain a subsurface image by means of the classical seismic analyses and the surface technique. Surface seismic reflection is aimed to obtain image of the first intervals of the subsurface, some texts refers it like high resolution seismic or surface seismic. The high resolution seismic is incorporated due small dimension of the structures, for determining - by this method - when it is compared to conventional seismic acquisition it is possible to establish geological structures deeper (1 to 10 km) with geological features of the surface seismic (lower than 800 m).


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