LIAG
Geological Structures
With seismic, magnetic and gravimetric methods we image subsurface structures. Depending on the method, the results vary in resolution and the parameters that are determined. The combination of 2D or 3D P- and S-wave seismics with magnetic and gravimetric investigations allows for an improved and far reaching interpretation. This is important for reservoir characterisation and geodynamic interpretation.
Reflection seismic structural image of a Quaternary Valley (black line) in combination with the distribution of specific electric resistivity from transient electromagnetics (colour code: orange to red - sand; light blue - clayey cover; green to yellow - glacial till; dark blue - Tertiary clay; nach Wiederhold et al. 2008).