Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/14675
Authors: Bigi, Sabina* 
Beaubien, Stanley Eugene* 
Ciotoli, Giancarlo* 
D’Ambrogi, Chiara* 
Doglioni, Carlo* 
Ferrante, V.* 
Lombardi, Salvatore* 
Milli, S.* 
Orlando, Luciana* 
Ruggiero, Livio* 
Tartarello, Maria Chiara* 
Sacco, Pietro* 
Title: Mantle-derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy)
Journal: Tectonophysics 
Series/Report no.: /637 (2014)
Publisher: Elsevier
Issue Date: 2014
DOI: 10.1016/j.tecto.2014.10.001
Keywords: soil gas
Fluid migration
Subject Classification04.04. Geology 
Abstract: Fluid migration along faults can be highly complex and spatially variable, with the potential for channeled flow, accumulation in capped porous units, fault cross-flow, lateral migration along strike, or complete sealing. Extensional basin margins can be important for such migration, given the associated crustal thinning and decompression that takes place combined with potential geothermal or mantle gas sources. One such example is near the urban area of Rome, situated along the active extensional continental margin of the Tyrrhenian back arc basin and surrounded by Middle-Upper Pleistocene K-rich and arc-related volcanoes. Recent research activities in the area around Fiumicino, a town 25 km to the west of Rome, has highlighted the close spatial link between degassing CO2 and the faults that provide the necessary vertical migration pathways. In particular, detailed soil gas and gas flux surveys have highlighted the release at surface of large volumes of asthenospheric mantle CO2 in correspondence with normal faults observed in a new seismic reflection profile acquired along the Tiber River. Detailed reconstruction of the Pleistocene–Holocene stratigraphy of the area dates fault activity from 20,000 to 9000 years BP. It is proposed that the gas migrates preferentially along the cataclastic tectonic breccias of the faults until it encounters recent, unconsolidated sediments; porous units within this shallow stratigraphy act as temporary secondary traps for the leaking gas, with local gas release at the ground surface occurring where the sealing of the overlying aquitards has been compromised. Degassing and active faults confirm the extensional tectonics affecting the area and the geodynamic scenario of a mantle wedge beneath the western Apennines, associated with ongoing W-directed subduction. Moreover, degassing highlights the potential geochemical and seismic risks for the highly populated urban areas near Rome.
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