Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10897
Authors: Quattrocchi, Fedora* 
Favara, Rocco* 
Capasso, Giorgio* 
Pizzino, Luca* 
Bencini, R.* 
Cinti, Daniele* 
Galli, Gianfranco* 
Grassa, Fausto* 
Francofonte, S.* 
Volpicielli, G.* 
Title: Thermal anomalies and fluid geochemistry framework in occurrence of the 2000-2001 Nizza Monferrate seismic sequence (northern Italy): Episodic changes in the fault zone heat flow or chemical mixing phenomena?
Journal: Natural Hazards and Earth System Science 
Series/Report no.: /3(2003)
Issue Date: 2003
Abstract: The paper discusses the correlation between the heating of shallow groundwater over a 10 × 20 km wide area close to the town of Nizza Monferrato (Piemonte Region, Northern Italy) and the concomitant local seismic sequences during the period August 2000 – July 2001. The first seismic sequence started on 21 August 2000 with a Ml = 5.2 earthquake. Within few hours, the local authorities received calls alerting that the groundwater temperature rose from 10 to 30°C in many shallow wells. Our geochemical experimental data and the geological-seismotectonic framework do not allow the hypothesis of simple fluid mixing between the thermal reservoir of Acqui Terme and the Nizza-Monferrato shallow groundwater to explain the observed thermal anomalies. On the other hand, we invoke more complex processes such as frictional heating, mechano-chemistry, fault-valve mechanism, adiabatic decompression and hydrogeologically driven heat flow i.e., thermal effects due to variations of basin-scale permeability field. All these processes are able to transmit heat to the surface and to generate a transient incremental heat flow better than the mass transfer occurring typically when fluids from different reservoirs mix
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