INTERPRETATION OF GEOCHEMICAL DATA FROM FUMAROLES AND WELLS IN THE NÁMAFJALL GEOTHERMAL FIELD, ICELAND AND FROM FUMAROLES IN THE MUTNOVSKY GEOTHERMAL FIELD, KAMCHATKA, RUSSIA
Sergey V. Ushakov
Abstract
Sergey V. Ushakov
Abstract
The Namafjall area is a high-temperature geothermal area in North Iceland. In this report data from 1989, 1995 and 1999 for two production wells are used to calculate mineral equilibria and for comparison with actual temperatures, measured in the wells. Some data from fumaroles in this field are used to compare calculated gas geothermometer temperatures with measured temperatures. Gas geothermometer temperatures were also calculated for fumaroles in the Mutnovsky geothermal field (southern part of Kamchatka peninsula, Far East Russia) for comparison with
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The Namafjall area is a high-temperature geothermal area in North Iceland. In this report data from 1989, 1995 and 1999 for two production wells are used to calculate mineral equilibria and for comparison with actual temperatures, measured in the wells. Some data from fumaroles in this field are used to compare calculated gas geothermometer temperatures with measured temperatures. Gas geothermometer temperatures were also calculated for fumaroles in the Mutnovsky geothermal field (southern part of Kamchatka peninsula, Far East Russia) for comparison with
Key concepts: Fumarole, Geothermal gradient, Geology, Volcano, Geothermal energy, Field (mathematics), Geochemistry, Mineralogy