Kwon, Tae-Hyuk; Cho, Gye-Chun - In: Energies 5 (2012) 8, pp. 2849-2873
sediments, thermal dissociation of gas hydrates, excess pore pressure generation, pressure diffusion, and hydrate dissociation …, by gas hydrate dissociation. It has been reported that during the past 55 years (1955–2010) the 0–2000 m layer of oceans … bottom water of deep oceans continues, it would dissociate natural gas hydrates and could eventually trigger massive slope …