The basic triggering mechanism underlying induced seismicity traces back to the mid‐1960s
that relied on the process of pore‐fluid pressure diffusion. The last decade has experienced …

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 …

The 2006 second edition of this well received and widely adopted textbook has been
extensively revised to provide a more comprehensive treatment of hydromechanics (the …

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 …

The temporal and spatial pattern of seismicity associated with reservoir water level
fluctuations, injection of high‐pressure fluids in deep boreholes, and seasonal groundwater …

A review of coupled groundwater and heat transfer theory is followed by an introduction to
geothermal measurement techniques. Thereafter, temperaturedepth profiles (geotherms) …

Coseismic static stress changes and dynamic stresses generated by seismic waves cause
changes in water level in wells and in stream flow and alter hydrogeologic properties such …

Abstract The Yellowstone Plateau Volcanic Field is characterized by extensive seismicity,
episodes of uplift and subsidence, and a hydrothermal system that comprises more than …

Mud volcanoes sometimes erupt within days after nearby earthquakes. The number of such
nearly coincident events is larger than would be expected by chance and the eruptions are …

Delineation of physical factors that contribute to earthquake triggering is a challenging issue
in seismology. We analyze hydrological modulation of seismicity in Taiwan using …