Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5838
AuthorsChiodini, G. 
TitleCO2/CH4 ratio in fumaroles a powerful tool to detect magma degassing episodes at quiescent Volcanoes
Issue Date17-Jan-2009
Series/Report no./36(2009)
DOI10.1029/2008GL036347
URIhttp://hdl.handle.net/2122/5838
KeywordsCO2/CH4
magma degassing
quiescent volcanoes
Subject Classification03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gases 
03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systems 
04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistry 
AbstractLong time series of fumarolic compositions at Campi Flegrei (Italy), Mammoth Mountain (California), Panarea (Italy) and Nisyros (Greece) show rapid increases, up to orders of magnitude, of the CO2/CH4 ratio systematically with the occurrence of volcanic unrest periods. These easily detected anomalies originate with the arrival of CH4-poor magmatic fluids in the shallower levels of the volcanoes. The data suggest that volcanoes are characterized by magmatic activity at depth also in periods of apparent quiescence. The activity is constituted by the pulsing release of large amount of fluids which either cause unrest periods (seismicity and ground deformation) or possibly could precede volcanic eruption. This type of volcanic activity can be monitored trough the classical geophysical techniques together with the systematic sampling and analysis of fumaroles.
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