2009
DOI: 10.1016/j.marpetgeo.2009.01.016
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A predictive numerical model for potential mapping of the gas hydrate stability zone in the Gulf of Cadiz

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Cited by 13 publications
(9 citation statements)
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“…This corroborates Leon et al [23] assertion that, in some of the mud volcanoes, the biogenic origin of part of the gas hydrates should not be discarded.…”
Section: Co2 Hydrate Stabilitysupporting
confidence: 89%
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“…This corroborates Leon et al [23] assertion that, in some of the mud volcanoes, the biogenic origin of part of the gas hydrates should not be discarded.…”
Section: Co2 Hydrate Stabilitysupporting
confidence: 89%
“…The raster datasets of geothermal gradient (δg), seafloor pressure (Psf) and seafloor temperature (Tsf) used in COHydrate are shown in Figure 4 and were derived by Bernardes et al [5], although the geothermal gradient dataset was updated using data listed in Benazzouz [29]. The maximum Lsz thickness of 798 m (Figure 4d) was found to be in agreement with the values computed by Leon et al [23], and by Peter R. Miles (725 m) as quoted by [29], but contrasts with the 550 m depth estimated by Benazzouz [29].…”
Section: Thickness Of Gas Hydrates Stability Zone (Lsz)supporting
confidence: 73%
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