Oscillations in stress, such as those created by earthquakes, can increase permeability and
fluid mobility in geologic media. In natural systems, strain amplitudes as small as 10− 6 can …

Terra Nova, 23, 145–161, 2011 Abstract The hydrogeology of superficial (∼ 0–100 m bgl)
Hard Rock Aquifers (HRA; ie plutonic and metamorphic rocks) has so far been dominated by …

Forests in tectonically active regions are disturbed by earthquakes. Besides direct injuries to
trees, earthquakes also induce stand-wide changes in hydrological conditions, whose …

The frictional resistance on a fault during slip controls earthquake dynamics. Friction
dissipates heat during an earthquake; therefore, the fault temperature after an earthquake …

Permeability controls fluid flow in fault zones and is a proxy for rock damage after an
earthquake. We used the tidal response of water level in a deep borehole to track …

Geofluids (2010) 10, 193–205 Abstract The variation of permeability with depth can be
probed indirectly by various means, including hydrologic models that use geothermal data …

It is generally accepted that tectonic earthquakes may trigger volcanic activity, although the
underlying mechanisms are poorly constrained. Here, we review current knowledge, and …

Injecting fluids in the crust, or their extraction, changes pore pressure and poroelastic
stresses. Both pressure and stress changes can promote seismicity and, hence, the seismic …

Groundwater chemistry has been observed to change before earthquakes and is proposed
as a precursor signal. Such changes include variations in radon count rates,, concentrations …

В монографии приведены результаты многолетних исследований закономерностей
деформирования нарушений сплошности массивов горных пород. На основе …