Technical Committee Earth Sciences

Active Tectonics in Northwest Germany: Glacial Isostatic Adjustment and/or a Consequence of Hydrocarbon Production?

The aim of the DGMK project 773 was to analyse trigger mechanisms for the recent earthquakes in NW Germany in order to better differentiate between potential anthropogenic and natural tectonic drivers. Possible trigger mechanisms are stress changes related to either the extraction of natural gas and/ or process of the ongoing glacial isostatic adjustment. The project was divided into three major parts: (i) seismological analyses; (ii) geological 3-D subsurface modeling and (iii) numerical simulations of the glacial isostatic adjustment.
In a novel approach, two differently scaled 3-D P-wave-velocity models were used in NonLinLoc to relocate seismic events in NW Germany. Focal mechanisms were created with GOCAD and used to visualize subsurface structures. Relocated hypocenters were linked with these sub-surface structures to identify seismogenic active faults. Subsequently, numerical simulations with six different rheology models were carries out by Holger Steffen (Landmäteriet, Gävle, Sweden) to test the probability for GIA-induced erathqueakes in GM Germany.
Most of the seismic events in NW Germany, which are ranging in depths between 5 and 9 km are concentrated along the Rotliegend rift normal faults in close proximity to the natural gas fields. Due to their spatio-temporal occurence and their similarities to other anthropogenic seismicity all over the world, they are most likely caused by the natural gas extraction. Driving forces for slightly stronger earthquakes (ML ≥ 4.0) of greater depth seem to be more complex. The Rotenburg mainshock from 2004 is possibly related to an interaction between major GIA-induced stress changes and a minor depletion triggered component.
Controlling factors for the deep earthquakes in northern Germany are difficult to derive. However, our results clearly indicate that also GIA-induced stress changes as a result of the melting of the Late Pleistocene ice sheet play a role in case of fault reactivation in the study area.