1887

Abstract

In the crystalline system groundwater circulate through fractures and fissures. Geophysical methods are commonly used to investigate. In this paper we present the preliminary results of a geoelectrical survey conducted at Barro Branco sub basin, São José do Ubá county. We collected geoelectrical data at 3 profiles. Data were processed and interpreted with a 1D inversion scheme. Two main aquifer system were identified: sedimentary and cristalline.

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/content/papers/10.3997/2214-4609-pdb.160.SBGF166
2005-09-11
2024-04-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.160.SBGF166
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