Author/Authors :
Porkhial، Soheil نويسنده Geothermal Energy Bureau, P.O.Box 14665-1169, Tehran-Iran , , Nouraliee، Javad نويسنده Geothermal Energy Bureau, P.O.Box 14665-1169, Tehran-Iran , , Rahmani، Mohammad Reza نويسنده , , Ebrahimi، Davar نويسنده Geothermal Energy Bureau, P.O.Box 14665-1169, Tehran-Iran ,
Abstract :
Vartun geothermal region (VGR) is located in west central part of Iran, 300 km in the
southeast of Tehran. VGR area is 277 km2and there are some geothermal surface
manifestations such as warm springs and travertine deposits. There are three warm springs
which their temperature varies from 35.3 to 43.1 °C. Their pH is a little bit acidic and is
about 6.1-6.2. Based on geothermometery studies Vartun geothermal reservoir
approximate temperature was estimated 46-182 °C. According to the geological,
aeromagnetic and remote sensing studies VGR probable reservoir and cap rock was
recognized. Therefore Permian dolomite, limestone and sandstone were regarded as
reservoir rock while cap rock includes shale and quartzite. Thermal energy of Vartun
geothermal resource was estimated 1.14 × 1017kj.