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Mantle derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy) (Articolo in rivista)
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- Label
- Mantle derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy) (Articolo in rivista) (literal)
- Anno
- 2014-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.tecto.2014.10.001 (literal)
- Alternative label
Bigi S., Beaubien S.E., Ciotoli G., D'Ambrogi C., Doglioni C., Ferrante V., Lombardi S., Milli S., Orlando L., Ruggiero L., Tartarello M.C., Sacco P. (2014)
Mantle derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy)
in Tectonophysics (Amst. Online)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bigi S., Beaubien S.E., Ciotoli G., D'Ambrogi C., Doglioni C., Ferrante V., Lombardi S., Milli S., Orlando L., Ruggiero L., Tartarello M.C., Sacco P. (literal)
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- http://www.sciencedirect.com/science/article/pii/S0040195114005150 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
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- Dipartimento di Scienze della Terra, SAPIENZA Università di Roma, P.le A. Moro, 5, 00185 Roma, Italy
IGAG-CNR Istituto di Geologia Ambientale e Geoingegneria, Area della Ricerca Roma 1, Via Salaria km 29.300, 00016 Monterotondo Stazione Roma, Italy
Istituto di Scienze Marine, ISMAR-CNR, Via Gobetti 101, 40129 Bologna, Italy
Dipartimento di Ingegneria Civile, Edile e Ambientale, SAPIENZA Università di Roma, Via Eudossiana 18, 00184 Roma, Italy (literal)
- Titolo
- Mantle derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy) (literal)
- 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 CO 2 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. (literal)
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