Mantle-derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy)-Reference-Cited by-同舟云学术

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Mantle-derived CO2 migration along active faults within an extensional basin margin (Fiumicino, Rome, Italy)

Published:2014-12 Issue: Volume:637 Page:137-149
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

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.

Funder

Sapienza University

Regione Lazio

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference66 articles.

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2. Gas migration along fault systems and through the vadose zone in the Latera caldera (central Italy): implications for CO2 geological storage;Annunziatellis;Int. J. Greenhouse Gas Control,2008

3. The deepstructure of the Eolian arc (Filicudi–Panarea–Vulcano Sector) in light of gravity, gravity, magnetic and volcanological data. Volcanological data;Barberi;J. Volcanol. Geotherm. Res.,1994

4. Gas blowout from shallow boreholes at Fiumicino (Rome): induced hazard and evidence of deep CO2 degassing on the Tyrrhenian margin of Central Italy;Barberi;J. Volcanol. Geotherm. Res.,2007

5. Carbon dioxide and radon gas hazard in the Alban Hills area (Central Italy);Beaubien;J. Volcanol. Geotherm. Res.,2003

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