In some North German gas fields, small earthquakes have occurred within or in the immediate vicinity of the reservoir during the production phase, while other gas fields show no seismicity. Previous studies (e.g. APIS 1) have used numerical simulations to identify some factors that generally favor the occurrence of critical stress states on faults within the reservoir or at its rim, which can ultimately result in earthquake activity. DGMK project 825 is dedicated to the question whether for individual natural gas fields there is indeed a correlation between the occurrence of seismicity and the geological factors favoring fault reactivation. Different types of reservoirs in the North German Basin, which differ in particular in their subsurface geometry and stratigraphic age, are considered.