Modelling geothermal conditions in part of the Szczecin Trough – the Chociwel area
The Chociwel region is part of the Szczecin Trough and constitutes the northeastern segment of the extended Szczecin-Gorzów Synclinorium. Lower Jurassic reservoirs of high permeability of up to 1145 mD can discharge geothermal waters with a rate exceeding 250 m3/h and temperatures reach over 90°C in...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Sciendo
2015-09-01
|
| Series: | Geologos |
| Subjects: | |
| Online Access: | https://doi.org/10.1515/logos-2015-0013 |