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Cascadia Margin

IODP Preliminary Report Leg 311 (Northern Cascadia Margin)... [Pg.3]

IODP Expedition 311 Scientists, Cascadia Margin gas hydrates. IODP Prel. Rept., 311. doi 10 2204/iodp. pr.311. (2005). [Pg.34]

P9a Northern Cascadia Margin Samples and Spence(1992) Pohlman et al. (2005)... [Pg.548]

Hydrate formation from gas dissolution of rising water Hyndman and Davis (1992) proposed that as methane-unsaturated water rises, it becomes saturated at lower pressures. As the saturated (or supersaturated) water passes through the phase stability zone, hydrate formation occurs without a free gas zone. This model results in a maximum hydrate concentration at the three-phase (BSR) boundary with a successively lower hydrate amounts above the BSR as was shown to be the case in Cascadia Margin ODP Drill Sites 889 and 890 by Hyndman et al. (1996). [Pg.565]

Table 7.7 contrasts FHF and DLF hydrates. It should be emphasized that both hydrates are end-member types with the frequent occurrence of mixed types. For example, while Table 7.7 typifies Blake Ridge as DLF hydrates and Barkley Canyon as FHF hydrates, there is often a mixture of both types as shown in the Leg 204 study in the Cascadia Margin. As a second example, while the Gulf of Mexico is normally known for FHF hydrate deposits, Hutchinson et al. (2004) provide evidence for some elements that have DLF characteristics. [Pg.566]

P9 Cascadia Margin off Vancouver 30 km wide band, 300 m subbottom Hyndman and Spence (1992) Yuan et al. (1996)... [Pg.575]

P8 Cascadia Margin off Oregon 73 m subbottom depth undefined area Westbrook et al. (1994)... [Pg.575]

Luff, R., Wallmann, K., 2003. Fluid flow, methane fluxes, carbonate precipitation and biogeochemical turnover in gas hydrate-bearing sediments at Hydrate Ridge, Cascadia Margin Numerical modeling and mass balances. Geochim. Cosmochim. Acta 67 (18), 3403-3421. [Pg.336]

Heeschen, K., Trehu, A., Collier, R.W., Suess, E., and Rehder, G, 2003. Distribution and height of methane bubble plumes on the Cascadia Margin characterized by acoustic imaging Geophysical Research Letters, 30 10.1029/2003GL016974. [Pg.509]

Torres, M.E., Wallmann, K., Trehu, A.M., Bohrmann, G, Borowski, W.S., and Tomaru, H., 2004. Gas hydrate growth, methane transport, and chloride enrichment at the southern summit of Hydrate Ridge, Cascadia margin off Oregon. Earth and Planetary Science Letters, 226 225-241. [Pg.511]

Westbrook, G.K., Carson, B., Musgrave, R.J., et al. 1994. Proceedings, initial reports. Ocean Drilling Program, Leg 146 Cascadia Margin, 611 pp. [Pg.512]


See other pages where Cascadia Margin is mentioned: [Pg.49]    [Pg.23]    [Pg.25]    [Pg.208]    [Pg.352]    [Pg.573]    [Pg.596]    [Pg.472]    [Pg.1995]    [Pg.1996]    [Pg.438]    [Pg.486]    [Pg.497]    [Pg.497]    [Pg.497]    [Pg.498]    [Pg.503]    [Pg.511]    [Pg.715]    [Pg.383]   
See also in sourсe #XX -- [ Pg.3 , Pg.23 , Pg.25 , Pg.34 , Pg.208 , Pg.352 , Pg.548 , Pg.565 , Pg.566 , Pg.573 , Pg.575 , Pg.596 ]




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Margin

Marginalization

Margining

Northern Cascadia Margin

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