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Universite de Montpellier II, Laboratoire GBE Equipe Hydrogeologie, Montpellier, France
This work presents the tectonic and seismic conditions of water level changes in a confined aquifer, in Armenia. The deviatoritic stress induces an extensive tectonic regime characterized by a E-W horizontal extension. The strain release at the time of a local earthquakes induces permeability and/or porosity changes, and so anomalies on the piezometry records.
This record provided courtesy of AGI/GeoRef.
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