Abstract Knowledge of the present-day crustal in-situ stress field is a key for the
understanding of geodynamic processes such as global plate tectonics and earthquakes. It …

Earthquakes can change the stress field in the Earth's lithosphere as they relieve and
redistribute stress. Earthquake‐induced stress changes have been observed as temporal …

Stress inversions from focal mechanisms require knowledge of which nodal plane is the
fault. If such information is missing, and faults and auxiliary nodal planes are interchanged …

In this contribution, we present a review of scientific research results that address seismo-
hydromechanically coupled processes relevant for the development of a sustainable heat …

This paper summarizes the current state of understanding regarding the induced seismicity
in connection with hydraulic fracturing operations targeting the Duvernay Formation in …

The estimation of the stress-field orientation from focal mechanisms of earthquakes is a
relevant tool to understand crustal mechanics and the physics of earthquakes. In global …

Geologic carbon storage, as well as other geo-energy applications, such as geothermal
energy, seasonal natural gas storage and subsurface energy storage imply fluid injection …

The spatiotemporal, kinematic, and source characteristics of induced seismicity occurring at
different fluid injection rates are investigated to determine the predominant physical …

Pore pressure increase associated with the injection of fluids in rock masses often generates
some microseismicity. But pore pressure variations depend on fluid diffusion, which itself …

The long‐term temporal and spatial changes in statistical, source, and stress characteristics
of one cluster of induced seismicity recorded at The Geysers geothermal field (US) are …