First page    Previous    Next    Index

 

Hungary



Geological setting, geothermal conditions 

 

Basin formation: Early-Middle Miocene crustal extension  

 

Streched (thinned lithosphere) 

 


High heat flux (90-100 mW/m²) – continental average (60 mW/m²).

Geothermal gradient  45 °C/km (World average: 20-25 °C/km) 

 

 

 


 

 

2 major geothermal reservoirs
- Karstified fractured-eathered zones
(Palaeozoic-Mesozoic basement carbonates):
- Multilayered porous sediments 
(Upper Miocene-Pliocene “Pannonian” basin fill sequence) : 

intergranular / porous reservoirs: best: delta (shelf) front sands

 

 

Current utilization

 

Red line: provisional contour of the DARLINGe area

 

Red line: provisional contour of the DARLINGe area

 

  • Agriculture: major sector for direct heat utilization (greenhouses, plastic tents)

  • Industrial purposes: few wells, typical outflow temperature is 40-50 °C

  • Balneological: ~255 wells, 40-50 °C outflow temperature

  • District heating: 21 towns in 2016 (thermal water heating cascade system)

    First page    Previous    Next    Index