RT Journal Article
T1 Análisis de la geometría en profundidad de fracturas conductoras en zonas de baja permeabilidad mediante tomografía eléctrica (El Berrocal, Sistema Central Español)
A1 Muñoz Martín, Alfonso
A1 Olaiz Campos, Antonio José
A1 Vicente Muñoz, Gerardo De
A1 Antón López, Loreto
A1 Elorza, Francisco José
A1 Vicente, Raquel de
AB The groundwater flow in zones of low permeability, as granites, is mainly associated with zones of fracture.For this reason the characterization of the fractures is fundamental, both in surface as in depth, and mustintegrate geological information (geological mapping, structural analysis), geophysics (mainly electricaland electromagnetic methods) and geochemistry (radon and others gases) with hydrogeology. In this work we analyze the geophysical response of a strike-slip fault zone by means of three 2D resistivity models. The objective is to investigate the presence of several conductive zones and their geometry in depth. The obtained results allow to control the geometry in depth of the fractures, the gaps between the different mapped traces along the fault zone as well as the thickness of landfill. All this information will be useful for the hidromechanical simulation of the massif, and to check the geometry and gas permeability calculated from emanometry.
PB Sociedad Geológica de España
SN 0213-683X
YR 2007
FD 2007
LK https://hdl.handle.net/20.500.14352/52678
UL https://hdl.handle.net/20.500.14352/52678
LA spa
DS Docta Complutense
RD 8 ago 2024