Abstract
The article presents the results of multi-year comprehensive geochemical and geophysical studies concerned with the caldera of the Golovnin volcano. The chemical composition of thermal solutions and condensates are discussed. Geophysical data within sections including discharge zones of geothermal waters associated with gas from hot springs were interpreted to examine the formation of chemical composition of fumarole gases and thermal solutions. The quantitative composition of the interacting media was identified and physicochemical models were built based on the actual data. Considering these models and the results of studying the subsurface area of thermal fields, the most probable physicochemical conditions for fluid ascent from depth to the surface are proposed.
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