Record Details

Title Volcanology and Geothermal Research by Using Hydrothermal Alteration Processes of Well NWS-4 at Sabalan Volcano Geothermal Project, Iran
Authors Zahed Mousavi, Ali Darvishzadeh
Year 2010
Conference World Geothermal Congress
Keywords Geothermal, Alteration minerals, Mt. Sabalan, Meshkin shahr, Iran
Abstract The Mt. Sabalan Hypabbusal basement batholiths with monzogranite compenent have been replaced inside of Eocene volcanic rocks during Miocene-Pliocene. Due to this replacement other suitable geological and hydrological conditions, a geothermal reservoir has been formed around Mt. Sabalan. Based on resistivity surveys combined with other geological & geochemical data, the area at N-W Sabalan located 20 km to south of Meshkin shahr was selected for geothermal exploration drilling. The well NWS-4 is one of the three exploration wells in this area. The result of studies show that an alteration system at NWS-4 has neutral pH & alteration zones consist of average argillic, phyllic & propylitic. In addition, by correlating extent temperature stability of alteration minerals for approximate well thermometry, the alteration temperature can be estimated to be 240 °C.
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