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From
Application of Seal Integrity and Fault Connectivity Analysis in Selecting Suitable Subsurface Geological Sites for Carbon Capture and Storage
Josephine Maximus, Livinus Nosike
Journal of Geosciences and Geomatics
.
2024
, 12(2), 24-35 doi:10.12691/jgg-12-2-1
Figure 1
.
Tectonostratigraphic Evolution of Guyana basin
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Figure 2
.
An Analogous comparison between Offshore Guyana and Offshore Niger Delta
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Figure 3
.
Methods of study – from regional to local seismic cross section and maps, through to correlation of stratigraphic units on which sealing parameters are tested
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Figure 4
.
Schema showing the throw in a geologic unit with sandstone (yellow) and shale (grey) intervals on the foot and hanging wall of a normal fault
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Figure 5
.
Fault zone showing very low permeabilities in turbiditic deposits of outcrops in the Annot Sandstone
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Figure 6
.
Tight and loose microfabrics similar to observation in fault zone and fault wall respectively
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Figure 7
.
Case fault X in the Niger Delta turbidites was modeled to show impact of burial and fault zone property on sealing potential
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Figure 8
.
Guyana Basin showing similar depositional architecture with incised values and basin floor reservoir lobes (usually offset by faults to form trap compartments
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Figure 9
.
Plot of contact angle against effective stress
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Figure 10
.
Impact of Burial on Fault Zone Hydraulic Property
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Figure 11
.
Structural profile showing depleted Well-X and Well-Y adjacent to the storage compartments in the Njak and Opoto prospective storage sites
Full size figure and legend