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Geo- and hydro-acoustic manifestations of shallow gas and gas seeps in the Dnepr paleodelta, northwestern Black Sea
Naudts, L.; De Batist, M.; Greinert , J.; Artemov, Y. (2009). Geo- and hydro-acoustic manifestations of shallow gas and gas seeps in the Dnepr paleodelta, northwestern Black Sea. Lead. Edge (Tulsa Okla.) 28(9): 1030-1040. dx.doi.org/10.1190/1.3236372
In: Leading Edge (Tulsa, Okla.). Society of Exploration Geophysicists: Tulsa, Okla.. ISSN 1070-485X; e-ISSN 1938-3789
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Keyword
    Marine/Coastal
Authors  Top 
  • Naudts, L.
  • De Batist, M.
  • Greinert, J.
  • Artemov, Y.
Abstract
    Shallow gas occurs between 0 and 1000 m below the sea floor. It consists mainly of microbial-formed or thermogenic methane or a combination of both, sometimes with a limited admixture of higher hydrocarbons (propane, butane, etc.).
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