Dr. Thomas Reichel - IASS Potsdam

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12 -Gas Hydrate Indications on the Mid-NorwayContinental Marginfrom Plaza-Faverola et al. 2010bResults• evidence for thermogenicsources• migration along deep seatedpolygonal faults• gas hydrates act as “broken”seal• Migration can reach seabedto from large ventsites/pockmarksResources• Huge GIP ~ 150-1400 GSm 3• Poor reservoir quality• Low (0,2 GSm 3 /km 2 )resource density,~ comparable to similarhydrate provinces
Gas Hydrate StabilityConditions in theBarents Sea• CH 4 hydrate probably not stable• Presence of BSR and hydratesample suggest thermogenicgas sourceRemaining issues:• Geothermal gradient?• Reservoir?Thickness of GHSZfrom Chand et al. (2008)13 -
Page 1 and 2: Gas Hydrate as a Resource- Statoil
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Page 5 and 6: Gas-hydrate-bearing sands seem the
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Page 15 and 16: Gas Hydrate potential on SvalbardMi
Page 17 and 18: Western Svalbard Margin Resource As
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Page 21 and 22: Thank youGas Hydrate as a Resource-

Dr. Thomas Reichel - IASS Potsdam

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