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- W2187521874 abstract "Fracture characterization in granites has been an important subject of study during these last years, by means of geological-structural cartography, hydrogeology and geochemical analysis. These works have been carried out to investigate the hydromechanics and permeability in low-permeability rocks. In this study we apply a surface geophysical method in order to characterize the permeability of the fault zones affecting «El Berrocal» granite (Central System, Spain). The low-induction electromagnetic method (EM) gives us the apparent resistivity (ρ a ) values of the rocks at a maximum depth. As the ρ a depends on the granite alteration and/or the water content, this parameter allows estimating the relative permeability of different fracture zones. The obtained results show that the high-permeability fractures are those that are larger ones which were active during Alpine deformation (Eocene-present)." @default.
- W2187521874 created "2016-06-24" @default.
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- W2187521874 date "2009-01-01" @default.
- W2187521874 modified "2023-10-18" @default.
- W2187521874 title "Aplicación del método electromagnético de inducción ligera para el análisis de la permeabilidad en medios fracturados (granito de El Berrocal, Sistema Central Español) Application of the low-induction electromagnetic method for the permeability analysis in fractured rocks («El Berrocal» granite, Spanish Central System)" @default.
- W2187521874 cites W2136312009 @default.
- W2187521874 hasPublicationYear "2009" @default.
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