Physics
Scientist
School of Earth & Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA
Co-existence of gas hydrate, free gas, and brine within the regional gas hydrate stability zone at Hydrate Ridge (Oregon margin): evidence from prolonged degassing of a pressurized core
Comment on “Gas hydrate growth, methane transport, and chloride enrichment at the southern summit of Hydrate Ridge, Cascadia margin off Oregon” by Torres et al. [Earth Planet. Sci. Lett. 226 (2004) 225 241]
The dynamics of submarine geothermal heat pipes
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