The Weisweiler passive seismological network: optimised for state-of-the-art location and imaging methods

Passive seismic analyses are a key technology for the exploration and monitoring of subsurface reservoirs. Searching for alternative resources in the framework of the energy transition is creating a surge for identifying as many potential sites as possible suitable for geothermal exploitation. The Lower Rhine Embayment, at the western border of North Rhine-Westphalia in Germany, is an extensional system with a very high potential for geothermal exploitation. The area experiences moderate but continuous natural seismicity. Here, we report on a passive seismic dataset recorded with 48 seismic stations centred at and around Eschweiler-Weisweiler (, Finger et al., 2022). Background seismic noise levels are high at this site due to high levels of anthropogenic noise and thick unconsolidated sedimentary layers. The final station layout is a compromise between targeted network design and suitably quiet locations. We show that the network design allows for the application of state-of-the-art methods including waveform-based source location methods and ambient-noise velocity imaging methods.

Automated summary

Passive seismic analyses are crucial for exploring and monitoring subsurface reservoirs. The Lower Rhine Embayment in Germany has a high potential for geothermal exploitation and experiences continuous natural seismicity. We present a passive seismic dataset recorded at Eschweiler-Weisweiler, showing that the network design allows for state-of-the-art analysis methods.