Seismic Methods in Geothermal Water Resource Exploration: Case Study from Łódź Trough, Central Part of Poland

<div>Thickness map of J<sub>2</sub>-T<sub>3</sub>k depth interval corresponding to cumulative thickness of Rhaetian, Lower Jurassic, and Middle Jurassic.</div>

Geofluids

fig6

Figure 6

Figure 6: Seismic Methods in Geothermal Water Resource Exploration: Case Study from Łódź Trough, Central Part of Poland 