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Articles

Methane-flow system within the Nyegga pockmark field, offshore mid-Norway

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By Umr Geo-Ocean, Umr Locean, Umr Beep, Marzia Rovere
| Frontiers
1 Introduction Pockmarks are commonly interpreted as sites of hydrodynamic removal of sediment caused by focused fluid discharge through the seabed (Judd and Hovland, 2007). Mainly associated with light hydrocarbon gases, pockmarks, since their first discovery off Nova Scotia (King and MacLean, 1970) have been identified and studied worldwide at numerous continental margins, in particular offshore Norway (Vogt et al., 1999b).
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