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Abstract

This paper shows the results of joint inversion of VES/TEM for Urupês region, Paraná sedimentary basin, São Paulo State, Brazil. The objectives of this research were to map the Adamantina Formation (sedimentary aquifer) and to locate fractures zones in the basalt layer of the Serra Geral Formation. The results indicate the tick of the Adamantina Formation (Bauru aquifer) and the fracture zones in the basalt of the Serra Geral Formation. Keywords: VES, TEM, Joint inversion, Paraná basin, Urupês, São Paulo State, Brazil.

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/content/papers/10.3997/2214-4609.20131389
2013-09-09
2024-04-19
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