2011
DOI: 10.1144/1354-0793/10-026
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The role of stratigraphic juxtaposition for seal integrity in proven CO 2 fault-bound traps of the Southern North Sea

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Cited by 30 publications
(14 citation statements)
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“…Upper Cretaceous, Tertiary and Quaternary sediments are thickest in the eastern part of the study area near the UK-Netherlands median line. Structural inversion during the Late Cretaceous resulted in contractional reactivation of existing deep-seated normal faults to the south of the Zechstein salt basin, and at least two later stages of structural inversion occurred as a result of Alpine events (Badley et al 1989;Yielding et al 2011). The Zechstein evaporites are widely characterised by halokinesis which initiated during the latter parts of the Triassic and continued intermittently throughout the Mesozoic (Allen et al 1994).…”
Section: Geological Settingmentioning
confidence: 99%
“…Upper Cretaceous, Tertiary and Quaternary sediments are thickest in the eastern part of the study area near the UK-Netherlands median line. Structural inversion during the Late Cretaceous resulted in contractional reactivation of existing deep-seated normal faults to the south of the Zechstein salt basin, and at least two later stages of structural inversion occurred as a result of Alpine events (Badley et al 1989;Yielding et al 2011). The Zechstein evaporites are widely characterised by halokinesis which initiated during the latter parts of the Triassic and continued intermittently throughout the Mesozoic (Allen et al 1994).…”
Section: Geological Settingmentioning
confidence: 99%
“…1,3,10,11 However, scCO 2 -although denser than CO 2 gas -is buoyant compared to formation water and migrates upwards; this migration can be minimized and CO 2 can be prevented from escaping to the atmosphere by four main trapping mechanisms: structural, [11][12][13] residual, 10,14,15 dissolution, [16][17][18] and mineral. [19][20][21] Many factors affect the efficiency and capacity of the main CO 2 trapping mechanisms: temperature, 22 vertical to horizontal permeability ratio, 23 cap rock properties, 13 fault-seal behaviour, 24,25 or reservoir heterogeneity. 26 One factor, which has received little attention, is the CO 2 -wettability of the rock.…”
Section: Introductionmentioning
confidence: 99%
“…An interesting find is the Fizzy gas field (UK) and the analogue Oak Field (discovered before 2007), both having a fault-dip closure configuration on the Fizzy Horst (Yielding et al 2011). Both fields contain extremely high CO 2 percentages, up to 50% for the Fizzy Field.…”
Section: New Geological Insights and Discoveries Since 2007mentioning
confidence: 99%