Depth estimation of fumarolic gas source deduced by fume pressure measurement
The origin of fumarolic gas is hydrothermal boiling in the active fumarolic area and magma degassing in the active volcano where high temperature gas is discharged. The determination of the fumarolic gas source is important for understanding the geothermal activity or the eruption process. However,...
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Veröffentlicht in: | Earth, planets, and space planets, and space, 2008-01, Vol.60 (8), p.889-893 |
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