Potential Geothermal Reservoirs in Hungary

This dataset contains layers showing the spatial distribution and/or depth of the horizon, below which thermal water of a certain temperature is likely to occur within the said sedimentary succession.

Quaternary porous reservoirs:
Quaternary 30-50 °C top
Quaternary 30-50 °C bottom
Upper-Pannonian porous reservoirs:
Upper-Pannonian 30-50 °C top
Upper-Pannonian 30-50 °C bottom
Upper-Pannonian: 50-75 °C top
Upper-Pannonian 50-75 °C bottom
Upper-Pannonian 75-100 °C top
Upper-Pannonian 75-100 °C bottom
Upper-Pannonian 100-125 °C top
Upper-Pannonian 100-125 °C bottom
Upper-Pannonian higher than 125 °C top
Upper-Pannonian higher than 125 °C bottom

Distribution of a certain temperature within the Pre-Cenozoic top:
The estimated temperature of the pre-Cenozoic basement is 120 °C based on a conductive model
The estimated temperature of the pre-Cenozoic basement is 150 °C based on a conductive model