Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6015
AuthorsChiodini, G.* 
Avino, R.* 
Caliro, S.* 
Cardellini, C.* 
Costa, A.* 
Frondini, F.* 
TitleCarbon dixide emission in Italy: Shallow crustal sources or subduction related fluid recycling?
Issue Date21-Jun-2009
URIhttp://hdl.handle.net/2122/6015
Keywordsanomalous flux CO2
Italy
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 
AbstractAnomalous non-volcanic CO2 release in central and southern Italy has been highlighted by ten years of detailed investigations on Earth degassing processes. Two regional degassing structures are located in the Tyrrhenian sector where more then 200 emissions of CO2 are located and has been recently included in the first web based catalogue of degassing sites (http://googas.ov.ingv.it). The total amount of CO2 released by the two structures were evaluated to be > 2×1011 mol a-1 ( >10% of the estimated global volcanic CO2 emission). The anomalous flux of CO2 suddenly disappears in the Apennine in correspondence of a narrow band where most of the Italian seismicity concentrates. Here, at depth, the gas accumulates in crustal traps generating CO2 overpressurised reservoirs. These overpressured structures are, in our opinion, one of the main cause of Apennine earthquake activation processes. The results of these investigations suggested that Earth degassing in Italy may have an active primary role in the geodynamics of the region. What is the origin of gas? The large extension of the degassing structures and petrologic data suggested that the main source of gas is a mantle metasomatised by the fluids produced in the subdacted slabs. However, has been also hypothesised the presence of localised crustal source of the gas. This matter will be discussed on the base of unpublished isotopic data of the main gas emissions.
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