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• W1980173190 abstract "The numerous CO 2 reservoirs in the Colorado Plateau region of the United States arenatural analogues for potential geologic CO 2 sequestration repositories. To betterunderstand the risk of leakage from reservoirs used for long-term underground CO 2 storage, we examine evidence for CO 2 migration along two normal faults from areservoir in east-central Utah. CO 2 -charged springs, geysers, and a hydrocarbon seepare localised along these faults. These include natural springs that have been active forlong periods of time, and springs that were induced by recent drilling. The CO 2 -chargedspring waters have deposited travertine mounds and carbonate veins. The faults cutsiltstones, shales, and sandstones and the fault rocks are fine-grained, clay-rich gouge,generally thought to be barriers to fluid flow. The geologic and geochemical data areconsistent with these faults being conduits for CO 2 to the surface. Consequently, theinjection of CO 2 into faulted geologic reservoirs, including faults with clay gouge, mustbe carefully designed and monitored to avoid slow seepage or fast rupture to thebiosphere." @default.
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• W1980173190 date "2004-01-01" @default.
• W1980173190 modified "2023-10-17" @default.
• W1980173190 title "Analysis of CO ₂ leakage through ‘low-permeability’ faults from natural reservoirs in the Colorado Plateau, east-central Utah" @default.
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• W1980173190 doi "https://doi.org/10.1144/gsl.sp.2004.233.01.05" @default.
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