ABSTRACT The 2016 M w 5.8 Pawnee earthquake occurred in a region with active
wastewater injection into a basal formation group. Prior to the earthquake, fluid injection …

Abstract Changes in groundwater or surface water level may cause observable deformation
of the drainage basins in different ways. We describe an active slope deformation monitored …

Rock deformation induced by pore‐fluid pressure carries useful information about fluid flow
owing to hydromechanical coupling. Thus, obtaining spatiotemporal changes in rock …

Abstract Space geodetic measurements from the Envisat satellite between 2003 and 2010
show that subsidence rates near the southeastern shoreline of the Salton Sea in Southern …

Strains occur at shallow depths in response to pressure changes during well tests in an
underlying aquifer, and recent developments in instrumentation have made it feasible to …

Storing and recovering water, carbon, and heat from geologic reservoirs is central to
managing resources in a changing climate. We tested the hypothesis that the strain tensor …

Karstic terrains are usually dominated by aquifer systems and/or underground cavities.
Overexploitation of groundwater in such areas often induces land subsidence and …

The elastic response of the lithosphere to surface mass redistributions produces
geodetically measurable deformation of the Earth. This deformation is especially …

Geodetic instruments now offer compelling sensitivity, allowing to investigate how solid
Earth and surface processes interact. By combining surface air pressure data, nontidal sea …

Triggered seismicity arising from dynamic stresses is often explained by the Mohr‐Coulomb
failure criterion, where elevated pore pressures reduce the effective strength of faults in fluid …