A Low Enthalpy Geothermal System in the Moesian Platform
- Key words
- carbonate aquifer, thermal water, geochemistry, origin, utilisation
- Location
- Moesian Platform; Romania
- Conference
- World Geothermal Congress
- Year
- 1995
- Session
- SECTION 4 ? Exploration and Conceptual Modeling
- Language
- English
- Paper number
- 2-Tenu
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Abstract
In the central part of the Moesian Platform in Romania there is a Mesozoic carbonate aquifer whose water temperatures are from 42oC to 80oC.
The goal of this paper is to describe the geothermal system origin of the water, peculiarity of the hydrothermalism and the stage of practical utilization.
The approach to these problems was by means of geochemical methods: hydrochemical analyses, specific conductivity and temperature measurements, environmental isotopic analyses (D, 18O, 3H, 14C).
Copyright 1995, International Geothermal Association. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.