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They are temporarily inhibited below an interpreted 300-m-thick gas hydrate layer marked by a strong BSR on seismic profiles.
The gas hydrate layer builds upward from the base of the stability zone with a thickness of less than 100 m.
Zone #2, which involved a gas hydrate layer with an underlying aquifer, could yield significant amounts of gas originating entirely from gas hydrates, the volumes of which increased with the production rate.
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Above the BSR, the velocity structure suggests the presence of gas hydrate in distinct layer from ~82 to 115 mbsf.
More gas hydrate occurrences and IS layers are identified in Hole C0008C, compared to Hole C0008A, but the total width covered by the IS layers is lesser (17.3 against 33.5 m).
The high-resistivity anomalies are correlated with a high-amplitude arrival in the seismic data at 1.3 s, which might be a gas hydrate-bearing layer within the gas hydrate stability zone.
So will be the gas hydrate horizons, by assuming the IS layers as potential reservoirs of gas hydrates.
When the CO2 hit the seawater, it developed a bizarre icy "hydrate" layer, through which the gas slowly dissolved.
Dense faults in the study area efficiently transport fluid from large depths to the shallow layer, supporting the formation of gas hydrate and ultimately the pockmark.
The exploitation of natural gas hydrate from the unconfined marine sediments, which is overlain by permeable layer, is challenging, as the traditional depressurization method cannot induce significant pressure drop in the hydrate reservoir to release the gas.
In the KG Basin gas hydrate in clay dominated sediment distributed in the form of layers, nodules, fracture-filling and pore filling was recovered from various well (Collett et al. 2008).
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